• prof. dr hab. Jerzy Żaba
Stanowisko: Profesor
Jednostka: Instytut Nauk o Ziemi
Adres: 41-200 Sosnowiec, ul. Będzińska 60
Piętro: IX
Numer pokoju: 919
Telefon: (32) 3689 434
E-mail: jerzy.zaba@us.edu.pl
Spis publikacji: Spis wg CINiBA
Spis publikacji: Spis wg OPUS
Scopus Author ID: 6602696411
Publikacje z bazy Scopus
2023
Moska, A.; Malczewski, D.; Żaba, J.; Dziurowicz, M.
In: Acta Montanistica Slovaca, vol. 28, no. 1, pp. 250-262, 2023, ISSN: 13351788.
@article{2-s2.0-85162787256,
title = {Natural radioactivity in select metamorphic and sedimentary rocks of the Opava Mountains (Poland): A comparison between laboratory and in situ measurements of232 Th,238 U, and40 K activities},
author = { A. Moska and D. Malczewski and J. Żaba and M. Dziurowicz},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85162787256&doi=10.46544%2fAMS.v28i1.20&partnerID=40&md5=055d6534201540064fa4c2760136b52f},
doi = {10.46544/AMS.v28i1.20},
issn = {13351788},
year = {2023},
date = {2023-01-01},
journal = {Acta Montanistica Slovaca},
volume = {28},
number = {1},
pages = {250-262},
publisher = {Technical University of Kosice},
abstract = {This paper reports the natural radioactivities of eight characteristic rocks from the Opava Mountains region (Eastern Sudetes; Poland) as measured in the laboratory and under in situ field conditions. Activity concentrations for232 Th,238 U, and40 K were obtained using an HPGe gamma-ray spectrometry system. Activities for232 Th ranged from 2 to 39 Bq kg−1 as measured in the laboratory and from 5 to 38 Bq kg−1 measured under in situ field conditions. For238 U, the activity concentrations ranged from 4 to 37 Bq kg−1 in the laboratory and from 7 to 42 Bq kg−1 under in situ field conditions. For40 K, activity concentrations ranged from 12 to 820 Bq kg−1 in the laboratory and from 60 to 826 Bq kg−1 under in situ field conditions. Measured activity concentrations were compared with average activity concentrations of radionuclides in similar types of rocks from different global localities. The in situ field measurement and laboratory measurements did not show significant differences indicating that both methods provide reliable232 Th,238 U, and40K results for different lithologies. © 2023 by the authors.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
This paper reports the natural radioactivities of eight characteristic rocks from the Opava Mountains region (Eastern Sudetes; Poland) as measured in the laboratory and under in situ field conditions. Activity concentrations for232 Th,238 U, and40 K were obtained using an HPGe gamma-ray spectrometry system. Activities for232 Th ranged from 2 to 39 Bq kg−1 as measured in the laboratory and from 5 to 38 Bq kg−1 measured under in situ field conditions. For238 U, the activity concentrations ranged from 4 to 37 Bq kg−1 in the laboratory and from 7 to 42 Bq kg−1 under in situ field conditions. For40 K, activity concentrations ranged from 12 to 820 Bq kg−1 in the laboratory and from 60 to 826 Bq kg−1 under in situ field conditions. Measured activity concentrations were compared with average activity concentrations of radionuclides in similar types of rocks from different global localities. The in situ field measurement and laboratory measurements did not show significant differences indicating that both methods provide reliable232 Th,238 U, and40K results for different lithologies. © 2023 by the authors.
2022
Michalak, M. P.; Teper, L.; Wellmann, F.; Żaba, J.; Gaidzik, K.; Kostur, M.; Maystrenko, Y. P.; Leonowicz, P.
Clustering has a meaning: optimization of angular similarity to detect 3D geometric anomalies in geological terrains Journal Article
In: Solid Earth, vol. 13, no. 11, pp. 1697-1720, 2022, ISSN: 18699510, (1).
@article{2-s2.0-85142623026,
title = {Clustering has a meaning: optimization of angular similarity to detect 3D geometric anomalies in geological terrains},
author = { M.P. Michalak and L. Teper and F. Wellmann and J. Żaba and K. Gaidzik and M. Kostur and Y.P. Maystrenko and P. Leonowicz},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85142623026&doi=10.5194%2fse-13-1697-2022&partnerID=40&md5=3f09f8d3280894dcbff7e63339430bf5},
doi = {10.5194/se-13-1697-2022},
issn = {18699510},
year = {2022},
date = {2022-01-01},
journal = {Solid Earth},
volume = {13},
number = {11},
pages = {1697-1720},
publisher = {Copernicus Publications},
abstract = {The geological potential of sparse subsurface data is not being fully exploited since the available workflows are not specifically designed to detect and interpret 3D geometric anomalies hidden in the data. We develop a new unsupervised machine learning framework to cluster and analyze the spatial distribution of orientations sampled throughout a geological interface. Our method employs Delaunay triangulation and clustering with the squared Euclidean distance to cluster local unit orientations, which results in minimization of the within-cluster cosine distance. We performed the clustering on two representations of the triangles: normal and dip vectors. The classes resulting from clustering were attached to a geometric center of a triangle (irregular version). We also developed a regular version of spatial clustering which allows the question to be answered as to whether points from a grid structure can be affected by anomalies. To illustrate the usefulness of the combination between cosine distance as a dissimilarity metric and two cartographic versions, we analyzed subsurface data documenting two horizons: (1) the bottom Jurassic surface from the Central European Basin System (CEBS) and (2) an interface between Middle Jurassic units within the Kraków-Silesian Homocline (KSH), which is a part of the CEBS. The empirical results suggest that clustering normal vectors may result in near-collinear cluster centers and boundaries between clusters of similar trend, thus pointing to axis of a potential megacylinder. Clustering dip vectors, on the other hand, resulted in near-co-circular cluster centers, thus pointing to a potential megacone. We also show that the linear arrangements of the anomalies and their topological relationships and internal structure can provide insights regarding the internal structure of the singularity, e.g., whether it may be due to drilling a nonvertical fault plane or due to a wider deformation zone composed of many smaller faults. Copyright © 2022 Michał P. Michalak et al.},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The geological potential of sparse subsurface data is not being fully exploited since the available workflows are not specifically designed to detect and interpret 3D geometric anomalies hidden in the data. We develop a new unsupervised machine learning framework to cluster and analyze the spatial distribution of orientations sampled throughout a geological interface. Our method employs Delaunay triangulation and clustering with the squared Euclidean distance to cluster local unit orientations, which results in minimization of the within-cluster cosine distance. We performed the clustering on two representations of the triangles: normal and dip vectors. The classes resulting from clustering were attached to a geometric center of a triangle (irregular version). We also developed a regular version of spatial clustering which allows the question to be answered as to whether points from a grid structure can be affected by anomalies. To illustrate the usefulness of the combination between cosine distance as a dissimilarity metric and two cartographic versions, we analyzed subsurface data documenting two horizons: (1) the bottom Jurassic surface from the Central European Basin System (CEBS) and (2) an interface between Middle Jurassic units within the Kraków-Silesian Homocline (KSH), which is a part of the CEBS. The empirical results suggest that clustering normal vectors may result in near-collinear cluster centers and boundaries between clusters of similar trend, thus pointing to axis of a potential megacylinder. Clustering dip vectors, on the other hand, resulted in near-co-circular cluster centers, thus pointing to a potential megacone. We also show that the linear arrangements of the anomalies and their topological relationships and internal structure can provide insights regarding the internal structure of the singularity, e.g., whether it may be due to drilling a nonvertical fault plane or due to a wider deformation zone composed of many smaller faults. Copyright © 2022 Michał P. Michalak et al.
Tyc, A.; Gaidzik, K.; Ciesielczuk, J.; Masías, P.; Paulo, A.; Postawa, A.; Żaba, J.
Thermal springs and active fault network of the central Colca River basin, Western Cordillera, Peru Journal Article
In: Journal of Volcanology and Geothermal Research, vol. 424, 2022, ISSN: 03770273, (1).
@article{2-s2.0-85125448690,
title = {Thermal springs and active fault network of the central Colca River basin, Western Cordillera, Peru},
author = { A. Tyc and K. Gaidzik and J. Ciesielczuk and P. Masías and A. Paulo and A. Postawa and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85125448690&doi=10.1016%2fj.jvolgeores.2022.107513&partnerID=40&md5=477bd07f9cfc539c6704bed449798733},
doi = {10.1016/j.jvolgeores.2022.107513},
issn = {03770273},
year = {2022},
date = {2022-01-01},
journal = {Journal of Volcanology and Geothermal Research},
volume = {424},
publisher = {Elsevier B.V.},
abstract = {Thermal waters and vapor discharges (hot springs; geysers; solfataras; and fumaroles) are common phenomena in volcanic regions at active plate boundaries, and the Central Andes are no exception. The Colca River basin in S Peru is a highly diversified and complex thermal region with unresolved questions on the origin of thermal fluids, reservoir temperature, and connections with tectonic and/or volcanic activity. To answer these, we used hydrogeochemical analysis of 35 water samples from springs and geysers, together with isotopic (δ18O and δD) analysis, chemical and mineral studies of precipitates collected in the field around these outflows, and field observations. We aimed (1) to recognize the geochemistry of thermal waters and precipitates in the central part of the Colca River basin, (2) to identify fluid sources and their origin, (3) to estimate the temperature of a potential geothermal reservoir, and (4) to discuss the regional active tectonic and volcanic framework of this geothermal region and mutual relationships. Our results corroborate a heterogeneous and complex geothermal system in the central part of the Colca River basin, with contrasting hydrogeochemical and physical properties, variable isotope composition, different reservoir temperatures, and associated precipitates around thermal springs. Processes controlling water chemistry are closely related to the Ampato-Sabancaya magmatic chamber's activity and tectonic structures that allow complex interactions of meteoric waters with magmatic fluids and gases. With a considerable gradient of pressure owing to local relief and deep incision in the Colca Canyon, these processes led to the differentiation of the thermal waters into three main groups. (1) Chloride-rich, mainly sodium chloride, thermal waters are of meteoric origin but mature within the geothermal reservoir possibly fed by magma degassing. These waters' chemical and isotopic composition results from water-rock interaction and mixing with magmatic waters within the reservoir. These waters discharge at the bottom of the Colca Canyon and Valley, presenting a broad hydrogeochemical spectrum and highly variable mineral phases precipitating at the outflows. The reservoir temperature estimated for these waters ranges from 180 to 200 °C. The group of hottest springs and geysers at the bottom of the Colca Canyon waters are fully equilibrated, with the reservoir temperature ~ 240 °C. (2) Sulfate-rich waters are shallow meteoric waters heated by ascending gases that form an independent group referring to the local water circulation, often controlled by tectonic barriers. (3) Bicarbonate-rich waters are the intermediate meteoric waters, divided into two hydrochemical groups: waters partially equilibrated with reservoir rocks and more similar to chloride-rich waters or additionally enriched with SO4 and more similar to sulfate-rich waters. Studied thermal springs show a clear spatial correlation with active and seismogenic crustal W- to NW-tracing normal and strike-slip faults. These act as barriers to infiltrating meteoric waters, provide pathways to hydrothermal solutions and gases assisting in meteoric water heating, and yield passages for pressured by lithostatic load and heated waters to ascend to the surface. © 2022},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Thermal waters and vapor discharges (hot springs; geysers; solfataras; and fumaroles) are common phenomena in volcanic regions at active plate boundaries, and the Central Andes are no exception. The Colca River basin in S Peru is a highly diversified and complex thermal region with unresolved questions on the origin of thermal fluids, reservoir temperature, and connections with tectonic and/or volcanic activity. To answer these, we used hydrogeochemical analysis of 35 water samples from springs and geysers, together with isotopic (δ18O and δD) analysis, chemical and mineral studies of precipitates collected in the field around these outflows, and field observations. We aimed (1) to recognize the geochemistry of thermal waters and precipitates in the central part of the Colca River basin, (2) to identify fluid sources and their origin, (3) to estimate the temperature of a potential geothermal reservoir, and (4) to discuss the regional active tectonic and volcanic framework of this geothermal region and mutual relationships. Our results corroborate a heterogeneous and complex geothermal system in the central part of the Colca River basin, with contrasting hydrogeochemical and physical properties, variable isotope composition, different reservoir temperatures, and associated precipitates around thermal springs. Processes controlling water chemistry are closely related to the Ampato-Sabancaya magmatic chamber's activity and tectonic structures that allow complex interactions of meteoric waters with magmatic fluids and gases. With a considerable gradient of pressure owing to local relief and deep incision in the Colca Canyon, these processes led to the differentiation of the thermal waters into three main groups. (1) Chloride-rich, mainly sodium chloride, thermal waters are of meteoric origin but mature within the geothermal reservoir possibly fed by magma degassing. These waters' chemical and isotopic composition results from water-rock interaction and mixing with magmatic waters within the reservoir. These waters discharge at the bottom of the Colca Canyon and Valley, presenting a broad hydrogeochemical spectrum and highly variable mineral phases precipitating at the outflows. The reservoir temperature estimated for these waters ranges from 180 to 200 °C. The group of hottest springs and geysers at the bottom of the Colca Canyon waters are fully equilibrated, with the reservoir temperature ~ 240 °C. (2) Sulfate-rich waters are shallow meteoric waters heated by ascending gases that form an independent group referring to the local water circulation, often controlled by tectonic barriers. (3) Bicarbonate-rich waters are the intermediate meteoric waters, divided into two hydrochemical groups: waters partially equilibrated with reservoir rocks and more similar to chloride-rich waters or additionally enriched with SO4 and more similar to sulfate-rich waters. Studied thermal springs show a clear spatial correlation with active and seismogenic crustal W- to NW-tracing normal and strike-slip faults. These act as barriers to infiltrating meteoric waters, provide pathways to hydrothermal solutions and gases assisting in meteoric water heating, and yield passages for pressured by lithostatic load and heated waters to ascend to the surface. © 2022
2021
Gaidzik, K.; Żaba, J.
Oriented rock samples for detailed structural analysis Book Chapter
In: pp. 715-723, Springer Science and Business Media Deutschland GmbH, 2021, ISSN: 21979545, (1).
@inbook{2-s2.0-85103158384,
title = {Oriented rock samples for detailed structural analysis},
author = { K. Gaidzik and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85103158384&doi=10.1007%2f978-3-030-60143-0_25&partnerID=40&md5=07db1154befcea8733d0580ba8d3fea6},
doi = {10.1007/978-3-030-60143-0_25},
issn = {21979545},
year = {2021},
date = {2021-01-01},
journal = {Springer Geology},
pages = {715-723},
publisher = {Springer Science and Business Media Deutschland GmbH},
abstract = {A significant part of the detailed structural analysis can be done in the field. However, in many cases, especially in studies on ductile shear zones, further in-depth microstructural analysis is needed. For this purpose, correct collection of oriented rock samples with various tectonic structures is crucial for legitimate structural analysis. Samples collected in the field with known spatial orientation permit the determination of various geometric and kinematic characteristics of the observed structures. Oriented samples collected from field also permit to note and interpret new, previously omitted and/or invisible structures that have not been noticed in the field. This article presents techniques useful for sample collection in the field, coordinate systems applicable in the structural studies, and methods to re-orientate samples, together with ways to select thin section orientation. These are essential steps toward detail structural analysis. © Springer Nature Switzerland AG 2021.},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {inbook}
}
A significant part of the detailed structural analysis can be done in the field. However, in many cases, especially in studies on ductile shear zones, further in-depth microstructural analysis is needed. For this purpose, correct collection of oriented rock samples with various tectonic structures is crucial for legitimate structural analysis. Samples collected in the field with known spatial orientation permit the determination of various geometric and kinematic characteristics of the observed structures. Oriented samples collected from field also permit to note and interpret new, previously omitted and/or invisible structures that have not been noticed in the field. This article presents techniques useful for sample collection in the field, coordinate systems applicable in the structural studies, and methods to re-orientate samples, together with ways to select thin section orientation. These are essential steps toward detail structural analysis. © Springer Nature Switzerland AG 2021.
2020
Gaidzik, K.; Żaba, J.; Ciesielczuk, J.
Tectonic control on slow-moving Andean landslides in the Colca Valley, Peru Journal Article
In: Journal of Mountain Science, vol. 17, no. 8, pp. 1807-1825, 2020, ISSN: 16726316, (4).
@article{2-s2.0-85088576085,
title = {Tectonic control on slow-moving Andean landslides in the Colca Valley, Peru},
author = { K. Gaidzik and J. Żaba and J. Ciesielczuk},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85088576085&doi=10.1007%2fs11629-020-6099-y&partnerID=40&md5=82e162c093a8cd84b274459ff6999d82},
doi = {10.1007/s11629-020-6099-y},
issn = {16726316},
year = {2020},
date = {2020-01-01},
journal = {Journal of Mountain Science},
volume = {17},
number = {8},
pages = {1807-1825},
publisher = {Science Press},
abstract = {The Colca Valley in the Central Andes is a region characterized by the occurrence of large slow-moving landslides and a high level of seismic activity. In this study, we aimed to determine passive and active tectonic control on the formation of selected five large landslides in the Colca Valley and to assess geohazard associated with these features. For that purpose, we performed a post-landslide field survey, applied remote sensing techniques, and obtained eyewitness accounts. Recently, the need to understand mass movement processes in this region is even higher due to the establishment of the Colca y Volcanes de Andagua Geopark (Colca and Andagua Volcanoes Geopark). Our results suggest that the studied landslides usually represent a complex failure mechanism, dominated by translational sliding or rotational displacements, commonly associated with the formation of horst-and-graben like structures. We found a spatial correlation between the distribution of landslides and inherited fault network. The head scarps appear to be limited by the WNW- to NW-striking faults, whereas the lateral extent of some of the reported features seems to be connected with the NNE-striking normal faults, common in both, the Mesozoic strata and the Pleistocene-Holocene deposits. © 2020, The Author(s).},
note = {4},
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pubstate = {published},
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}
The Colca Valley in the Central Andes is a region characterized by the occurrence of large slow-moving landslides and a high level of seismic activity. In this study, we aimed to determine passive and active tectonic control on the formation of selected five large landslides in the Colca Valley and to assess geohazard associated with these features. For that purpose, we performed a post-landslide field survey, applied remote sensing techniques, and obtained eyewitness accounts. Recently, the need to understand mass movement processes in this region is even higher due to the establishment of the Colca y Volcanes de Andagua Geopark (Colca and Andagua Volcanoes Geopark). Our results suggest that the studied landslides usually represent a complex failure mechanism, dominated by translational sliding or rotational displacements, commonly associated with the formation of horst-and-graben like structures. We found a spatial correlation between the distribution of landslides and inherited fault network. The head scarps appear to be limited by the WNW- to NW-striking faults, whereas the lateral extent of some of the reported features seems to be connected with the NNE-striking normal faults, common in both, the Mesozoic strata and the Pleistocene-Holocene deposits. © 2020, The Author(s).
Mazur, S.; Aleksandrowski, P.; Gągała, Ł.; Krzywiec, P.; Żaba, J.; Gaidzik, K.; Sikora, R.
Late Palaeozoic strike-slip tectonics versus oroclinal bending at the SW outskirts of Baltica: case of the Variscan belt’s eastern end in Poland Journal Article
In: International Journal of Earth Sciences, vol. 109, no. 4, pp. 1133-1160, 2020, ISSN: 14373254, (24).
@article{2-s2.0-85077678270,
title = {Late Palaeozoic strike-slip tectonics versus oroclinal bending at the SW outskirts of Baltica: case of the Variscan belt’s eastern end in Poland},
author = { S. Mazur and P. Aleksandrowski and Ł. Gągała and P. Krzywiec and J. Żaba and K. Gaidzik and R. Sikora},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85077678270&doi=10.1007%2fs00531-019-01814-7&partnerID=40&md5=4ae87843e8b55395b4a5ab1a7831c527},
doi = {10.1007/s00531-019-01814-7},
issn = {14373254},
year = {2020},
date = {2020-01-01},
journal = {International Journal of Earth Sciences},
volume = {109},
number = {4},
pages = {1133-1160},
publisher = {Springer},
abstract = {Geophysical and geological data from the eastern sector of the Central European Variscan belt are presented and reviewed in the regional tectonic context. Matched filtering of isostatic gravity, guided by results of spectral analysis, along with other derivatives of gravity and magnetic fields reveal a dominant WNW–ESE-trending pre-Permian structural grain in the external zones of the Variscan belt in Poland. This trend is confirmed by regional distribution of dips in Carboniferous and Devonian strata that were penetrated by boreholes beneath Permian-Mesozoic sediments. Based on these data, two alternative concepts explaining the connection of the Variscan belt and its NE foreland, those of strike-slip tectonics versus oroclinal bending, are discussed. The WNW–ESE structural trend in the Variscan foreland is parallel to a set of major strike-slip fault zones in the area, including those of Upper Elbe, Intra-Sudetic, Odra, Dolsk and Kraków-Lubliniec. These faults are considered to convey a significant dextral displacement between Laurussia and Gondwana. The revised position of the Variscan deformation front shows a similar, uninterrupted, generally WNW–ESE trend, up to the SE border of Poland, which indicates an initial continuation of the Variscan belt into the area of the present-day Western Carpathians. The geometry of the Variscan deformation front along with the pattern of the Variscan structural grain are inconsistent with the idea of an oroclinal loop affecting the external, non-metamorphic Variscan belt. However, the data presented do not entirely rule out an oroclinal loop within the Variscan internides. The still possible options are (1) a semi-oroclinal model postulating ~ 90° bending of the Variscan tectonostratigraphic zones into parallelism with the WNW–ESE strike-slip faults or (2) an orocline limited only to the belt linking the Wolsztyn High and Moravo-Silesian non- to weakly-metamorphic fold-and-thrust belt. Regardless of the kinematic model preferred, our data indicate that structural evolution of the Polish Variscides was concluded with the end-Carboniferous NNE–SSW shortening that resulted in the present-day extent of the Variscan deformation front. © 2020, The Author(s).},
note = {24},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Geophysical and geological data from the eastern sector of the Central European Variscan belt are presented and reviewed in the regional tectonic context. Matched filtering of isostatic gravity, guided by results of spectral analysis, along with other derivatives of gravity and magnetic fields reveal a dominant WNW–ESE-trending pre-Permian structural grain in the external zones of the Variscan belt in Poland. This trend is confirmed by regional distribution of dips in Carboniferous and Devonian strata that were penetrated by boreholes beneath Permian-Mesozoic sediments. Based on these data, two alternative concepts explaining the connection of the Variscan belt and its NE foreland, those of strike-slip tectonics versus oroclinal bending, are discussed. The WNW–ESE structural trend in the Variscan foreland is parallel to a set of major strike-slip fault zones in the area, including those of Upper Elbe, Intra-Sudetic, Odra, Dolsk and Kraków-Lubliniec. These faults are considered to convey a significant dextral displacement between Laurussia and Gondwana. The revised position of the Variscan deformation front shows a similar, uninterrupted, generally WNW–ESE trend, up to the SE border of Poland, which indicates an initial continuation of the Variscan belt into the area of the present-day Western Carpathians. The geometry of the Variscan deformation front along with the pattern of the Variscan structural grain are inconsistent with the idea of an oroclinal loop affecting the external, non-metamorphic Variscan belt. However, the data presented do not entirely rule out an oroclinal loop within the Variscan internides. The still possible options are (1) a semi-oroclinal model postulating ~ 90° bending of the Variscan tectonostratigraphic zones into parallelism with the WNW–ESE strike-slip faults or (2) an orocline limited only to the belt linking the Wolsztyn High and Moravo-Silesian non- to weakly-metamorphic fold-and-thrust belt. Regardless of the kinematic model preferred, our data indicate that structural evolution of the Polish Variscides was concluded with the end-Carboniferous NNE–SSW shortening that resulted in the present-day extent of the Variscan deformation front. © 2020, The Author(s).
2019
Żaba, J.; Gaidzik, K.
Variscan stress regime rotation: Insights from the analysis of kink folds in the northern margin of the Bohemian Massif, South Poland Journal Article
In: Comptes Rendus - Geoscience, vol. 351, no. 5, pp. 395-405, 2019, ISSN: 16310713, (1).
@article{2-s2.0-85067304645,
title = {Variscan stress regime rotation: Insights from the analysis of kink folds in the northern margin of the Bohemian Massif, South Poland},
author = { J. Żaba and K. Gaidzik},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85067304645&doi=10.1016%2fj.crte.2019.04.003&partnerID=40&md5=12c2e19cb9422bf7cbe4e49e1a7dc2c7},
doi = {10.1016/j.crte.2019.04.003},
issn = {16310713},
year = {2019},
date = {2019-01-01},
journal = {Comptes Rendus - Geoscience},
volume = {351},
number = {5},
pages = {395-405},
publisher = {Elsevier Masson SAS},
abstract = {We aimed to determine variations in stress regimes during the youngest Variscan deformations in the northern part of the Bohemian Massif. For this purpose, we calculated the orientation of the principal stress and strain axes for kink folds observed in the metamorphic envelope of the Karkonosze Granite, using two methods: 1) the traditional method, incorporating structural diagrams (for conjugate kink folds only), and 2) butterfly diagram analysis. The use of both methods enabled us to determine the stress regime, based not only on conjugate but also on monoclinal kink bands. The obtained results prove that butterfly diagram analysis, when applied to monoclinal kink folds, yields reliable results, especially when calibrated using the internal friction angle (Ф) calculated for the conjugate structures. We identified two generations of kink folds: 1) an older one, developed under sublatitudinal shortening and most probably related to the Early Carboniferous terminal stages of the northwest-directed thrusting of the metamorphic units, and 2) a younger one; produced by north-south Variscan Carboniferous compression, and the emplacement and subsequent doming of the Karkonosze Granite. This is the first study on brittle-ductile structures observed commonly in the metamorphic units of the Bohemian Massif, showing their relation to the granitoid intrusion and complementing the tectonic models that usually omit kink folds. © 2019 Académie des sciences},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
We aimed to determine variations in stress regimes during the youngest Variscan deformations in the northern part of the Bohemian Massif. For this purpose, we calculated the orientation of the principal stress and strain axes for kink folds observed in the metamorphic envelope of the Karkonosze Granite, using two methods: 1) the traditional method, incorporating structural diagrams (for conjugate kink folds only), and 2) butterfly diagram analysis. The use of both methods enabled us to determine the stress regime, based not only on conjugate but also on monoclinal kink bands. The obtained results prove that butterfly diagram analysis, when applied to monoclinal kink folds, yields reliable results, especially when calibrated using the internal friction angle (Ф) calculated for the conjugate structures. We identified two generations of kink folds: 1) an older one, developed under sublatitudinal shortening and most probably related to the Early Carboniferous terminal stages of the northwest-directed thrusting of the metamorphic units, and 2) a younger one; produced by north-south Variscan Carboniferous compression, and the emplacement and subsequent doming of the Karkonosze Granite. This is the first study on brittle-ductile structures observed commonly in the metamorphic units of the Bohemian Massif, showing their relation to the granitoid intrusion and complementing the tectonic models that usually omit kink folds. © 2019 Académie des sciences
Paulo, A.; Ciesielczuk, J.; Racki, G.; Żaba, J.; Gaidzik, K.
Polish Geological Institute, vol. 67, no. 3, 2019, ISSN: 00332151.
@proceedings{2-s2.0-85064381603,
title = {Depositional environment and probable source of detritus in the upper cretaceous red-bed ashua formation (Peru) [Srodowisko sedymentacji i domniemane zrodlo materialu detrytycznego w gornokredowej formacji red-bed Ashua (Peru)]},
author = { A. Paulo and J. Ciesielczuk and G. Racki and J. Żaba and K. Gaidzik},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85064381603&doi=10.7306%2f2019.17&partnerID=40&md5=fd1bf4d2612c0ca95c559b42b5bda9de},
doi = {10.7306/2019.17},
issn = {00332151},
year = {2019},
date = {2019-01-01},
journal = {Przeglad Geologiczny},
volume = {67},
number = {3},
pages = {189-191},
publisher = {Polish Geological Institute},
abstract = {Ashua Formation was deposited in Coniacian-Early Santonian time near shore of a shallow sea and in a plethora of continental arid environments. Its main component is fine-grained siliciclastic materialforming lithic and subordinate arkosic graywackes. Limestones are frequent in the lower member, and in the upper one gypsum and halite are present. Based on sedimentary textures and detailedpetrographic studies, nine general microfacies were identified: shallow sea, beach, brack'isch and mudflats, lagoon, sabkha and playa, deltaic, alluvial, mudflows, dunes at shoreline of an agitated water basin. The present authors suggest that the main source of detritus was pyroclastic deposits. They probably belong to the heavily eroded Lower Cretaceous Matalaque Formation. © 2019 Polish Geological Institute. All Rights Reserved.},
keywords = {},
pubstate = {published},
tppubtype = {proceedings}
}
Ashua Formation was deposited in Coniacian-Early Santonian time near shore of a shallow sea and in a plethora of continental arid environments. Its main component is fine-grained siliciclastic materialforming lithic and subordinate arkosic graywackes. Limestones are frequent in the lower member, and in the upper one gypsum and halite are present. Based on sedimentary textures and detailedpetrographic studies, nine general microfacies were identified: shallow sea, beach, brack'isch and mudflats, lagoon, sabkha and playa, deltaic, alluvial, mudflows, dunes at shoreline of an agitated water basin. The present authors suggest that the main source of detritus was pyroclastic deposits. They probably belong to the heavily eroded Lower Cretaceous Matalaque Formation. © 2019 Polish Geological Institute. All Rights Reserved.
Malczewski, D.; Żaba, J.
In situ gamma-ray measurements of40k,232th and238u in high-grade metamorphic rocks from the sowie mountains (Sudetes, SW Poland) Journal Article
In: Geological Quarterly, vol. 63, no. 3, pp. 493-504, 2019, ISSN: 16417291.
@article{2-s2.0-85075088111,
title = {In situ gamma-ray measurements of40k,232th and238u in high-grade metamorphic rocks from the sowie mountains (Sudetes, SW Poland)},
author = { D. Malczewski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85075088111&doi=10.7306%2fgq.1483&partnerID=40&md5=1eabd61bf5f2c80ec410f80e5aa1d90e},
doi = {10.7306/gq.1483},
issn = {16417291},
year = {2019},
date = {2019-01-01},
journal = {Geological Quarterly},
volume = {63},
number = {3},
pages = {493-504},
publisher = {Polish Geological Institute},
abstract = {This paper reports on the abundance of primordial radionuclides (40K;232Th and238U) in characteristic lithologies from the Sowie Mountains (SW Poland). In situ gamma-ray measurements were conducted at 12 localities hosting exposed augen gneiss, flaser gneiss, granulite, homophanized gneiss, hornblendite, layered gneiss, layered migmatite, migmatic gneiss, mylonitic gneiss and mylonitic granulite. The activity concentration of40K varied from 180 Bq kg–1 (mylonitic granulite) to 845 Bq kg–1 (layered gneiss). The activity concentrations associated with228Ac (232Th) varied from 10 Bq kg–1 (mylonitic granulite) to 53 Bq kg–1 (homophanized gneiss), while activity associated with226Ra (238U) varied from 9 Bq kg–1 (mylonitic granulite) to 43 Bq kg–1 (layered gneiss). An augen gneiss adjacent to the Intra-Sudetic Fault showed the highest combined Th + U activity (89 Bq kg–1). The average Th/U ratio (3.6) calculated for gneiss outcrops of the Sowie Mountains falls within the range reported for biotite gneiss (3.5–4). Subsurface outcrops from the Walim–Rzeczka underground complex did not give noticeably higher238U activities. The results obtained for the Sowie lithologies are compared with those obtained by similar methods for similar rocks as reported in literature sources. © 2019, Polish Geological Institute. All rights reserved.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
This paper reports on the abundance of primordial radionuclides (40K;232Th and238U) in characteristic lithologies from the Sowie Mountains (SW Poland). In situ gamma-ray measurements were conducted at 12 localities hosting exposed augen gneiss, flaser gneiss, granulite, homophanized gneiss, hornblendite, layered gneiss, layered migmatite, migmatic gneiss, mylonitic gneiss and mylonitic granulite. The activity concentration of40K varied from 180 Bq kg–1 (mylonitic granulite) to 845 Bq kg–1 (layered gneiss). The activity concentrations associated with228Ac (232Th) varied from 10 Bq kg–1 (mylonitic granulite) to 53 Bq kg–1 (homophanized gneiss), while activity associated with226Ra (238U) varied from 9 Bq kg–1 (mylonitic granulite) to 43 Bq kg–1 (layered gneiss). An augen gneiss adjacent to the Intra-Sudetic Fault showed the highest combined Th + U activity (89 Bq kg–1). The average Th/U ratio (3.6) calculated for gneiss outcrops of the Sowie Mountains falls within the range reported for biotite gneiss (3.5–4). Subsurface outcrops from the Walim–Rzeczka underground complex did not give noticeably higher238U activities. The results obtained for the Sowie lithologies are compared with those obtained by similar methods for similar rocks as reported in literature sources. © 2019, Polish Geological Institute. All rights reserved.
2018
Wójcik, E.; Zielińska, M.; Chybiorz, R.; Żaba, J.
Depositional architecture of marginal multiple-source ramp of the Magura Basin (Eocene Flysch formation, Outer Western Carpathians) Journal Article
In: Geologica Carpathica, vol. 69, no. 4, pp. 347-364, 2018, ISSN: 13350552, (2).
@article{2-s2.0-85051529536,
title = {Depositional architecture of marginal multiple-source ramp of the Magura Basin (Eocene Flysch formation, Outer Western Carpathians)},
author = { E. Wójcik and M. Zielińska and R. Chybiorz and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85051529536&doi=10.1515%2fgeoca-2018-0021&partnerID=40&md5=a20cf19b44fadf7ebda23fc4a5a20403},
doi = {10.1515/geoca-2018-0021},
issn = {13350552},
year = {2018},
date = {2018-01-01},
journal = {Geologica Carpathica},
volume = {69},
number = {4},
pages = {347-364},
publisher = {Sciendo},
abstract = {The Zembrzyce Beds were studied to interpret the environments and facies in the western part of the Siary Subunit. New sedimentological data were obtained for the reconstruction of the depositional architecture of the Zembrzyce Beds. Based on detailed facies analysis, 9 facies and 4 facies associations were recognized. The facies associations represent different architectural elements of a submarine fan, such as: termination of distributary channel with transition to depositional lobe (distal part of mid-fan/outer fan sub-deposystem), lobes and distal lobes (outer fan sub-deposystem). According to the classification of Reading & Richards (1994) the fan deposystem can be classified as mud/sand-rich ramp. This system consists of several elongated lobes that formed synchronously, migrated laterally, and then retreated or decayed. The depositional system was supplied from the north and north-east. The inner-fan sub-deposystem was not detected. The sediments were deposited by high- and low-density turbidity currents and hyper-concentrated density flows sensu Mulder & Alexander (2001) with participation of the depositional background processes (pelagic settling). The sedimentary conditions of the Zembrzyce Beds during the Late Eocene were controlled by tectonic movements, the progress of the subduction and the global sea level changes. © 2018 Ewa Wójcik et al., published by Sciendo 2018.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Zembrzyce Beds were studied to interpret the environments and facies in the western part of the Siary Subunit. New sedimentological data were obtained for the reconstruction of the depositional architecture of the Zembrzyce Beds. Based on detailed facies analysis, 9 facies and 4 facies associations were recognized. The facies associations represent different architectural elements of a submarine fan, such as: termination of distributary channel with transition to depositional lobe (distal part of mid-fan/outer fan sub-deposystem), lobes and distal lobes (outer fan sub-deposystem). According to the classification of Reading & Richards (1994) the fan deposystem can be classified as mud/sand-rich ramp. This system consists of several elongated lobes that formed synchronously, migrated laterally, and then retreated or decayed. The depositional system was supplied from the north and north-east. The inner-fan sub-deposystem was not detected. The sediments were deposited by high- and low-density turbidity currents and hyper-concentrated density flows sensu Mulder & Alexander (2001) with participation of the depositional background processes (pelagic settling). The sedimentary conditions of the Zembrzyce Beds during the Late Eocene were controlled by tectonic movements, the progress of the subduction and the global sea level changes. © 2018 Ewa Wójcik et al., published by Sciendo 2018.
Dżaluk, A.; Malczewski, D.; Żaba, J.; Dziurowicz, M.
Natural radioactivity in granites and gneisses of the Opava Mountains (Poland): a comparison between laboratory and in situ measurements Journal Article
In: Journal of Radioanalytical and Nuclear Chemistry, vol. 316, no. 1, pp. 101-109, 2018, ISSN: 02365731, (3).
@article{2-s2.0-85042122357,
title = {Natural radioactivity in granites and gneisses of the Opava Mountains (Poland): a comparison between laboratory and in situ measurements},
author = { A. Dżaluk and D. Malczewski and J. Żaba and M. Dziurowicz},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85042122357&doi=10.1007%2fs10967-018-5726-3&partnerID=40&md5=0d872a25e4175f036f7d772a6241a515},
doi = {10.1007/s10967-018-5726-3},
issn = {02365731},
year = {2018},
date = {2018-01-01},
journal = {Journal of Radioanalytical and Nuclear Chemistry},
volume = {316},
number = {1},
pages = {101-109},
publisher = {Springer Netherlands},
abstract = {The natural radioactivities of five characteristic igneous rocks of the eastern foreland of the Opava Mountains (Eastern Sudetes; Poland), obtained in the laboratory and under in situ conditions, are presented. The activity concentrations of 232Th, 238U, and 40K were measured using an HPGe gamma-ray spectrometry system. The ranges of the activity concentrations of 232Th were 7–71 Bq kg−1 in the laboratory and 6–68 Bq kg−1 for the in situ measurements. For 238U, the ranges of the activity concentrations were 5–52 Bq kg−1 in the laboratory and 9–48 Bq kg−1 for the in situ measurements, and for 40K, the ranges were 520–1560 Bq kg−1 in the laboratory and 537–1700 Bq kg−1 for the in situ measurements. These determined activity concentrations were compared with the average activity concentrations of the radionuclides in similar types of rocks and with data from the Sudetes available in the literature. No significant differences were found between the in situ and laboratory measurements. © 2018, The Author(s).},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The natural radioactivities of five characteristic igneous rocks of the eastern foreland of the Opava Mountains (Eastern Sudetes; Poland), obtained in the laboratory and under in situ conditions, are presented. The activity concentrations of 232Th, 238U, and 40K were measured using an HPGe gamma-ray spectrometry system. The ranges of the activity concentrations of 232Th were 7–71 Bq kg−1 in the laboratory and 6–68 Bq kg−1 for the in situ measurements. For 238U, the ranges of the activity concentrations were 5–52 Bq kg−1 in the laboratory and 9–48 Bq kg−1 for the in situ measurements, and for 40K, the ranges were 520–1560 Bq kg−1 in the laboratory and 537–1700 Bq kg−1 for the in situ measurements. These determined activity concentrations were compared with the average activity concentrations of the radionuclides in similar types of rocks and with data from the Sudetes available in the literature. No significant differences were found between the in situ and laboratory measurements. © 2018, The Author(s).
2017
Gaidzik, K.; Żaba, J.
In: Przeglad Geologiczny, vol. 65, no. 12, pp. 1548-1554, 2017, ISSN: 00332151, (2).
@article{2-s2.0-85040699498,
title = {Comparison of fold deformation sequences in the northern and southern metamorphic cover of the Karkonosze granitoids [Porownanie sekwencji deformacji faldowych w polnocnej i poludniowej okrywie granitoidow Karkonoszy]},
author = { K. Gaidzik and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85040699498&partnerID=40&md5=8296137dfd232e8e872a40729acf86a6},
issn = {00332151},
year = {2017},
date = {2017-01-01},
journal = {Przeglad Geologiczny},
volume = {65},
number = {12},
pages = {1548-1554},
publisher = {Polish Geological Institute},
abstract = {We applied the detailed structural analysis to 394 outcrops in the southern and northern metamorphic cover of the Karkonosze Intrusion.We recognised five generations of fold structures: F1 -poorly preserved tight inlrafoliation folds; F2 - the most common generation, with the whole variety of fold geometries, W-Eand WSW-ENE-orientedfold axes in the northern contact zone, and W-E and WNW-ESE-oriented fold axes in the southern contact zone; F3 - chevronfolds; F4 - kink folds observed only in the Stara Kam ienica schist belt; and F$ - wide open folds, locally transformed into monoclinal kink folds, probably formed during the Variscan intrusion of the Karkonosze pluton. Similarity observed in the structural style in the northern and southern contact zones prove that these lithostratigraphic units had formed a single unit - the Izera-Kowary Unit - and had undergone the same deformaiional stages before the Karkonosze granitoid intrusion took place.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
We applied the detailed structural analysis to 394 outcrops in the southern and northern metamorphic cover of the Karkonosze Intrusion.We recognised five generations of fold structures: F1 -poorly preserved tight inlrafoliation folds; F2 - the most common generation, with the whole variety of fold geometries, W-Eand WSW-ENE-orientedfold axes in the northern contact zone, and W-E and WNW-ESE-oriented fold axes in the southern contact zone; F3 - chevronfolds; F4 - kink folds observed only in the Stara Kam ienica schist belt; and F$ - wide open folds, locally transformed into monoclinal kink folds, probably formed during the Variscan intrusion of the Karkonosze pluton. Similarity observed in the structural style in the northern and southern contact zones prove that these lithostratigraphic units had formed a single unit - the Izera-Kowary Unit - and had undergone the same deformaiional stages before the Karkonosze granitoid intrusion took place.
Dziurowicz, M.; Malczewski, D.; Żaba, J.
222Rn and 220Rn concentrations in selected soils developed on the igneous rocks of the kaczawa mountains (Sudetes, Poland) Journal Article
In: Acta Montanistica Slovaca, vol. 22, no. 3, pp. 238-245, 2017, ISSN: 13351788, (1).
@article{2-s2.0-85037718948,
title = {222Rn and 220Rn concentrations in selected soils developed on the igneous rocks of the kaczawa mountains (Sudetes, Poland)},
author = { M. Dziurowicz and D. Malczewski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85037718948&partnerID=40&md5=02f3f739500e9a3bef434fab9e4cadf8},
issn = {13351788},
year = {2017},
date = {2017-01-01},
journal = {Acta Montanistica Slovaca},
volume = {22},
number = {3},
pages = {238-245},
publisher = {Technical University of Kosice},
abstract = {This study presents the preliminary results of 222Rn (radon) and 220Rn (thoron) concentrations that were measured in the soils developed on igneous rocks including mafic (pillow lavas; basalts and melaphyre) and acid (keratophyre; rhyolite and rhyolitic tuff) rocks at ten locations in the Kaczawa Mountains (SW Poland). The measurements were carried out at sampling depths of 10, 40 and 80 cm using a RAD7 portable radon system. The highest concentrations of radon (222Rn) were mainly observed in the soils overlaying acid igneous rocks. The highest value of 11 kBq m-3 was obtained at a depth of 10 cm for soils overlaying melaphyre. At depths of 40 and 80 cm, the averages of 222Rn concentrations showed the same values of 3.6 kBq m-3 for all of the soils investigated. The highest concentrations of thoron (220Rn) were observed in soils overlaying acid igneous rocks, i.e. the value of 49 kBq m-3 at a depth of 40 cm for soils overlaying rhyolitic tuff. In the soils developed on basalts, the average concentrations of 222Rn increased with the sampling depth, whereas the average concentrations of thoron (220Rn) decreased with increasing sampling depth. Positive correlations were found between 232Th activity in the parent rocks and soil gas 220Rn concentrations at all of the sampling depths, whereas a positive correlation between soil gas 222Rn and the 238U activity concentration in the parent rocks was only found at a depth of 40 cm. © 2017, Technical University of Kosice. All rights reserved.},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
This study presents the preliminary results of 222Rn (radon) and 220Rn (thoron) concentrations that were measured in the soils developed on igneous rocks including mafic (pillow lavas; basalts and melaphyre) and acid (keratophyre; rhyolite and rhyolitic tuff) rocks at ten locations in the Kaczawa Mountains (SW Poland). The measurements were carried out at sampling depths of 10, 40 and 80 cm using a RAD7 portable radon system. The highest concentrations of radon (222Rn) were mainly observed in the soils overlaying acid igneous rocks. The highest value of 11 kBq m-3 was obtained at a depth of 10 cm for soils overlaying melaphyre. At depths of 40 and 80 cm, the averages of 222Rn concentrations showed the same values of 3.6 kBq m-3 for all of the soils investigated. The highest concentrations of thoron (220Rn) were observed in soils overlaying acid igneous rocks, i.e. the value of 49 kBq m-3 at a depth of 40 cm for soils overlaying rhyolitic tuff. In the soils developed on basalts, the average concentrations of 222Rn increased with the sampling depth, whereas the average concentrations of thoron (220Rn) decreased with increasing sampling depth. Positive correlations were found between 232Th activity in the parent rocks and soil gas 220Rn concentrations at all of the sampling depths, whereas a positive correlation between soil gas 222Rn and the 238U activity concentration in the parent rocks was only found at a depth of 40 cm. © 2017, Technical University of Kosice. All rights reserved.
Malczewski, D.; Żaba, J.
222Rn and 220Rn concentrations in soil gas of the Izera Massif (Sudetes, Poland) as a function of sampling depth Journal Article
In: Geological Quarterly, vol. 61, no. 4, pp. 877-886, 2017, ISSN: 16417291.
@article{2-s2.0-85033364638,
title = {222Rn and 220Rn concentrations in soil gas of the Izera Massif (Sudetes, Poland) as a function of sampling depth},
author = { D. Malczewski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85033364638&doi=10.7306%2fgq.1377&partnerID=40&md5=6d53837e123c03f2ea072dc66caa9e61},
doi = {10.7306/gq.1377},
issn = {16417291},
year = {2017},
date = {2017-01-01},
journal = {Geological Quarterly},
volume = {61},
number = {4},
pages = {877-886},
publisher = {Polish Geological Institute},
abstract = {This research presents soil gas 222Rn and 220Rn concentrations measured at 17 locations in the Izera Massif of southwest Poland. The average 222Rn concentrations at sampling depths of 10, 40 and 80 cm were 8, 78 and 224 kBq m-3, respectively. The average 220Rn concentrations for the same depths (10; 40 and 80 cm) were 6, 10 and 13 kBq m-3, respectively. Profiles of the concentrations versus depth can be fitted by exponential, linear and polynomial functions for soils developed on fault zones, above uranium mineral deposits, and above faulted uranium deposits, respectively. Soils developed on bedrock without fault zones or uranium mineralisation exhibit concentrations that follow a power function with an exponent of p <1. © 2017, Polish Geological Institute. All rights reserved.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
This research presents soil gas 222Rn and 220Rn concentrations measured at 17 locations in the Izera Massif of southwest Poland. The average 222Rn concentrations at sampling depths of 10, 40 and 80 cm were 8, 78 and 224 kBq m-3, respectively. The average 220Rn concentrations for the same depths (10; 40 and 80 cm) were 6, 10 and 13 kBq m-3, respectively. Profiles of the concentrations versus depth can be fitted by exponential, linear and polynomial functions for soils developed on fault zones, above uranium mineral deposits, and above faulted uranium deposits, respectively. Soils developed on bedrock without fault zones or uranium mineralisation exhibit concentrations that follow a power function with an exponent of p <1. © 2017, Polish Geological Institute. All rights reserved.
Malczewski, D.; Jeleń, M.; Żaba, J.; Błachowski, A.; Ruebenbauer, K.; Dziurowicz, M.
Identification of iron-bearing minerals in basalts and pillow lavas of the Kaczawa Mountains using 57Fe Mössbauer spectroscopy Journal Article
In: Nukleonika, vol. 62, no. 2, pp. 145-148, 2017, ISSN: 00295922, (2).
@article{2-s2.0-85023162016,
title = {Identification of iron-bearing minerals in basalts and pillow lavas of the Kaczawa Mountains using 57Fe Mössbauer spectroscopy},
author = { D. Malczewski and M. Jeleń and J. Żaba and A. Błachowski and K. Ruebenbauer and M. Dziurowicz},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85023162016&doi=10.1515%2fnuka-2017-0021&partnerID=40&md5=42e7327d7bb5b3c60c781860d4fc7d6c},
doi = {10.1515/nuka-2017-0021},
issn = {00295922},
year = {2017},
date = {2017-01-01},
journal = {Nukleonika},
volume = {62},
number = {2},
pages = {145-148},
publisher = {Institute of Nuclear Chemistry and Technology},
abstract = {The Kaczawa Mountains along with the Kaczawa foothill comprise a complicated geological unit that is called the Kaczawa metamorphic (Sudetes; SW Poland). The aim of our work was to identify the iron-bearing minerals in samples of basalts and pillow lavas from the Kaczawa metamorphic using 57Fe Mössbauer spectroscopy. Based on the preliminary results, the Fe3+/Fe2+ ratio in the samples was determined. © 2017 Dariusz Malczewski et al.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Kaczawa Mountains along with the Kaczawa foothill comprise a complicated geological unit that is called the Kaczawa metamorphic (Sudetes; SW Poland). The aim of our work was to identify the iron-bearing minerals in samples of basalts and pillow lavas from the Kaczawa metamorphic using 57Fe Mössbauer spectroscopy. Based on the preliminary results, the Fe3+/Fe2+ ratio in the samples was determined. © 2017 Dariusz Malczewski et al.
2015
Matyszkiewicz, J.; Kochman, A.; Rzepa, G.; Gołębiowska, B.; Krajewski, M.; Gaidzik, K.; Żaba, J.
In: Acta Geologica Polonica, vol. 65, no. 2, pp. 181-203, 2015, ISSN: 00015709, (16).
@article{2-s2.0-84938351124,
title = {Epigenetic silicification of the Upper Oxfordian limestones in the Sokole Hills (Kraków-Czêstochowa Upland): Relationship to facies development and tectonics},
author = { J. Matyszkiewicz and A. Kochman and G. Rzepa and B. Gołębiowska and M. Krajewski and K. Gaidzik and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84938351124&doi=10.1515%2fagp-2015-0007&partnerID=40&md5=43d017ed11a5edf35b58fe5f325f9563},
doi = {10.1515/agp-2015-0007},
issn = {00015709},
year = {2015},
date = {2015-01-01},
journal = {Acta Geologica Polonica},
volume = {65},
number = {2},
pages = {181-203},
publisher = {Adam Mickiewicz University Press},
abstract = {A spectacular epigenetic silicification was encountered in the Oxfordian bedded limestones exposed in the Sokole Hills situated in the Krakow-Częstochowa Upland. The main epigenetic mineral is microcrystalline quartz accompanied by minor goethite, hematite, barite, galena and sphalerite. Locally, the mineralized limestones reveal Pb and Cu contents exceeding over 150 times the background values of these metals in unmineralized limestones. The epigenetic mineralization of the bedded limestones was probably a two-stage process. During the first, Early Cretaceous stage, silicified limestones formed at the erosional surface of a denuded carbonate complex. Such silicification greatly limited the progress of the first karstification phase of the Upper Jurassic carbonates initiated in the Hauterivian. The sources of silica accumulated in the limestones were descending solutions enriched in silica derived from the weathering zone. This silicification affected the topmost part of the Upper Jurassic massive limestones and the deeper portions of the bedded limestones along the fracture systems and stylolites. Early Cretaceous tectonic activity generated new dislocations and re-opened the existing faults, which were subsequently filled with permeable Albian quartz sands. These openings became the migration pathways for ascending, warm, relict, sulphide-carrying hydrothermal solutions at the second formation stage of the epigenetic mineralization. The newly supplied silica from the Albian sands precipitated on the silicified limestones and, as concentric rims, on brecciated, early diagenetic cherts. The second-stage mineralization proceeded under phreatic conditions, presumably close to a fluctuating mixing zone of ascending, warm hydrothermal solutions and descending cold groundwaters. The brecciated cherts acting as silica crystallization nuclei indicate that the last mineralization stage probably followed the final phase of Cenozoic faulting. © 2015 Acta Geologica Polonica.},
note = {16},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
A spectacular epigenetic silicification was encountered in the Oxfordian bedded limestones exposed in the Sokole Hills situated in the Krakow-Częstochowa Upland. The main epigenetic mineral is microcrystalline quartz accompanied by minor goethite, hematite, barite, galena and sphalerite. Locally, the mineralized limestones reveal Pb and Cu contents exceeding over 150 times the background values of these metals in unmineralized limestones. The epigenetic mineralization of the bedded limestones was probably a two-stage process. During the first, Early Cretaceous stage, silicified limestones formed at the erosional surface of a denuded carbonate complex. Such silicification greatly limited the progress of the first karstification phase of the Upper Jurassic carbonates initiated in the Hauterivian. The sources of silica accumulated in the limestones were descending solutions enriched in silica derived from the weathering zone. This silicification affected the topmost part of the Upper Jurassic massive limestones and the deeper portions of the bedded limestones along the fracture systems and stylolites. Early Cretaceous tectonic activity generated new dislocations and re-opened the existing faults, which were subsequently filled with permeable Albian quartz sands. These openings became the migration pathways for ascending, warm, relict, sulphide-carrying hydrothermal solutions at the second formation stage of the epigenetic mineralization. The newly supplied silica from the Albian sands precipitated on the silicified limestones and, as concentric rims, on brecciated, early diagenetic cherts. The second-stage mineralization proceeded under phreatic conditions, presumably close to a fluctuating mixing zone of ascending, warm hydrothermal solutions and descending cold groundwaters. The brecciated cherts acting as silica crystallization nuclei indicate that the last mineralization stage probably followed the final phase of Cenozoic faulting. © 2015 Acta Geologica Polonica.
Buła, Z.; Habryn, R.; Jachowicz-Zdanowska, M.; Żaba, J.
The precambrian and lower paleozoic of the brunovistulicum (eastern part of the upper silesian block, southern Poland) – The state of the art Journal Article
In: Geological Quarterly, vol. 59, no. 1, pp. 123-134, 2015, ISSN: 16417291, (19).
@article{2-s2.0-84933048982,
title = {The precambrian and lower paleozoic of the brunovistulicum (eastern part of the upper silesian block, southern Poland) – The state of the art},
author = { Z. Buła and R. Habryn and M. Jachowicz-Zdanowska and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84933048982&doi=10.7306%2fgq.1203&partnerID=40&md5=a0650942cf5733d4eacc976b768145a0},
doi = {10.7306/gq.1203},
issn = {16417291},
year = {2015},
date = {2015-01-01},
journal = {Geological Quarterly},
volume = {59},
number = {1},
pages = {123-134},
publisher = {Polish Geological Institute},
abstract = {The Precambrain basement and Lower Paleozoic (Cambrian–Ordovicuna) sedimentary cover in the eastern part of the Upper Silesian Block (Brunovistulicum), known only in boreholes, is presented, and their palaeogeographic, fancies and palaeotectonic development is discussed. The former is characterized by a heterogenous structure that consists of Arching-Lower Proterozoic and Neoproterozoic rocks of different lithologies and origins, and the latter is almost exclusively represented by marine, transitional and terrestrial siliciclastic rocks. In contrast to the neighboring region of the western part of the Ma³opolska Block, the siliciclastic sedimenstation took place during the Early and Middle Cambrian in this area, however, the Ordovician deposits were encountered in several boreholes and no Silurian rocks have been reported in the northern part of this region. The authors present the most probable model of sidementation, teconics and origin of the geological structure of the Lower Paleozoic sedimonetary cover in the Upper Silesian Block, define research problems, and justify the need for new drillings. Based on the geological and structural analysis of the depth to the top surface of the Lower Paleozoic, they define the optimal location for three 1500 m deep boreholes to solve the basic research problems. © 2015, Polish Geological Institute. All Rights Reserved.},
note = {19},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Precambrain basement and Lower Paleozoic (Cambrian–Ordovicuna) sedimentary cover in the eastern part of the Upper Silesian Block (Brunovistulicum), known only in boreholes, is presented, and their palaeogeographic, fancies and palaeotectonic development is discussed. The former is characterized by a heterogenous structure that consists of Arching-Lower Proterozoic and Neoproterozoic rocks of different lithologies and origins, and the latter is almost exclusively represented by marine, transitional and terrestrial siliciclastic rocks. In contrast to the neighboring region of the western part of the Ma³opolska Block, the siliciclastic sedimenstation took place during the Early and Middle Cambrian in this area, however, the Ordovician deposits were encountered in several boreholes and no Silurian rocks have been reported in the northern part of this region. The authors present the most probable model of sidementation, teconics and origin of the geological structure of the Lower Paleozoic sedimonetary cover in the Upper Silesian Block, define research problems, and justify the need for new drillings. Based on the geological and structural analysis of the depth to the top surface of the Lower Paleozoic, they define the optimal location for three 1500 m deep boreholes to solve the basic research problems. © 2015, Polish Geological Institute. All Rights Reserved.
2014
Stano, M.; Żaba, J.; Małolepszy, Z.
In: Przeglad Geologiczny, vol. 62, no. 12, pp. 846-847, 2014, ISSN: 00332151, (1).
@article{2-s2.0-84921823045,
title = {3D geological model of the Knurów-Szczyglowice hard coal deposit [Trójwymiarowy model geologiczny złoża węgla kamiennego KWK "Knurów-Szczygłowice"]},
author = { M. Stano and J. Żaba and Z. Małolepszy},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84921823045&partnerID=40&md5=4d3d5fdc8b3cdc0336610636fc767878},
issn = {00332151},
year = {2014},
date = {2014-01-01},
journal = {Przeglad Geologiczny},
volume = {62},
number = {12},
pages = {846-847},
publisher = {Polish Geological Institute},
abstract = {The paper describes a workflow (and a resulting 3D geological model), developed for detailed 3D modeling of coal deposits in the "Knurów-Szczyglowice" Underground Coal Mine in the Upper Silesian Coal Basin The model covers 20 sa. km (4 × 5 km) and integrates data from various sources mainly coal seam mining maps and lithological borehole profiles, but also auxiliaiy sources like legacy cross-sections and structural maps. High grid resolution and relatively small uncertainties allow future testing of the model's application in industiy-related issues such as mining subsidence prediction or underground coal gasification.},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The paper describes a workflow (and a resulting 3D geological model), developed for detailed 3D modeling of coal deposits in the "Knurów-Szczyglowice" Underground Coal Mine in the Upper Silesian Coal Basin The model covers 20 sa. km (4 × 5 km) and integrates data from various sources mainly coal seam mining maps and lithological borehole profiles, but also auxiliaiy sources like legacy cross-sections and structural maps. High grid resolution and relatively small uncertainties allow future testing of the model's application in industiy-related issues such as mining subsidence prediction or underground coal gasification.
2013
Ciesielczuk, J.; Żaba, J.; Bzowska, G.; Gaidzik, K.; Głogowska, M.
Sulphate efflorescences at the geyser near Pinchollo, southern Peru Journal Article
In: Journal of South American Earth Sciences, vol. 42, pp. 186-193, 2013, ISSN: 08959811, (18).
@article{2-s2.0-84871747604,
title = {Sulphate efflorescences at the geyser near Pinchollo, southern Peru},
author = { J. Ciesielczuk and J. Żaba and G. Bzowska and K. Gaidzik and M. Głogowska},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84871747604&doi=10.1016%2fj.jsames.2012.06.016&partnerID=40&md5=3eae045dda31e6dc113ab3290155cab2},
doi = {10.1016/j.jsames.2012.06.016},
issn = {08959811},
year = {2013},
date = {2013-01-01},
journal = {Journal of South American Earth Sciences},
volume = {42},
pages = {186-193},
abstract = {Sulphate mineralization precipitated around a geyser located above the village of Pinchollo, Chivay district and below Hualca Hualca volcano (6025 m a.s.l.) in the Western Cordillera of southern Peru is described. The geyser is one of many manifestations of thermal activity in the Arequipa department. Its age is estimated to be Upper Pleistocene-Holocene, as the discharge point lies at the intersection of a fault system with latitudinal dip-slip fault cutting a volcanic-debris avalanche of probably Pleistocene age. Thermal waters present in the Chivay district are mainly chloride-rich with a neutral pH. They are rich in Li, Sr, and B. The water erupting in the geyser boils at about 85 °C, as it lies at some 4353 m a.s.l.The minerals examined, of various habits and various yellow, orange and white colours were precipitated on the soil and on plants close to the geyser (location 1), on the walls of a 1 m diameter pothole filled with boiling water (location 1a) and at a distance of some 100 m to the west of the geyser (location 2). All are sulphates. Their chemical composition is fairly simple, consisting of Al, Fe, K, Mg, Ca, S, NH4 and O, and all display chemical zoning. But the phase composition is more complex. In all locations, alunogene, copiapite, coquimbite, tschermigite and gypsum are present. Close to the geyser (location 1) magnesium-containing sulphates, namely, boussingaultite and pickeringite also occur. Iron sulphates such as mohrite and rozenite precipitate on the walls of the pothole (location 1a). Sulphates containing potassium such as jarosite, alunite and voltaite-voltaite (Mg) dominate among the efflorescences in location 2, where hematite was also noted. Any quartz and kaolinite or illite/mica admixture identified in some samples derives from adjacent soil.The present geothermal system does not involve the deposition of precious-metal deposits such as those associated with an earlier deep-going epithermal system that scavenged a large volume of rock. Most likely, as the present-day thermal waters do not involve a juvenile-water component, the geyser waters derive from a shallower source. © 2012 Elsevier Ltd.},
note = {18},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Sulphate mineralization precipitated around a geyser located above the village of Pinchollo, Chivay district and below Hualca Hualca volcano (6025 m a.s.l.) in the Western Cordillera of southern Peru is described. The geyser is one of many manifestations of thermal activity in the Arequipa department. Its age is estimated to be Upper Pleistocene-Holocene, as the discharge point lies at the intersection of a fault system with latitudinal dip-slip fault cutting a volcanic-debris avalanche of probably Pleistocene age. Thermal waters present in the Chivay district are mainly chloride-rich with a neutral pH. They are rich in Li, Sr, and B. The water erupting in the geyser boils at about 85 °C, as it lies at some 4353 m a.s.l.The minerals examined, of various habits and various yellow, orange and white colours were precipitated on the soil and on plants close to the geyser (location 1), on the walls of a 1 m diameter pothole filled with boiling water (location 1a) and at a distance of some 100 m to the west of the geyser (location 2). All are sulphates. Their chemical composition is fairly simple, consisting of Al, Fe, K, Mg, Ca, S, NH4 and O, and all display chemical zoning. But the phase composition is more complex. In all locations, alunogene, copiapite, coquimbite, tschermigite and gypsum are present. Close to the geyser (location 1) magnesium-containing sulphates, namely, boussingaultite and pickeringite also occur. Iron sulphates such as mohrite and rozenite precipitate on the walls of the pothole (location 1a). Sulphates containing potassium such as jarosite, alunite and voltaite-voltaite (Mg) dominate among the efflorescences in location 2, where hematite was also noted. Any quartz and kaolinite or illite/mica admixture identified in some samples derives from adjacent soil.The present geothermal system does not involve the deposition of precious-metal deposits such as those associated with an earlier deep-going epithermal system that scavenged a large volume of rock. Most likely, as the present-day thermal waters do not involve a juvenile-water component, the geyser waters derive from a shallower source. © 2012 Elsevier Ltd.
2012
Żaba, J.; Małolepszy, Z.; Gaidzik, K.; Ciesielczuk, J.; Paulo, A.
Fault network in Rio Colca valley between Maca and Pinchollo, Central Andes, southern Peru Journal Article
In: Annales Societatis Geologorum Poloniae, vol. 82, no. 3, pp. 279-290, 2012, ISSN: 02089068, (13).
@article{2-s2.0-84873479272,
title = {Fault network in Rio Colca valley between Maca and Pinchollo, Central Andes, southern Peru},
author = { J. Żaba and Z. Małolepszy and K. Gaidzik and J. Ciesielczuk and A. Paulo},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84873479272&partnerID=40&md5=b8822f6de70661eb09921ac2c45c97a8},
issn = {02089068},
year = {2012},
date = {2012-01-01},
journal = {Annales Societatis Geologorum Poloniae},
volume = {82},
number = {3},
pages = {279-290},
abstract = {The network of faults andjoints within the Mesozoic, Miocene and Pleistocene-Holocene formations was studied in the Rio Colca valley, in the Pinchollo-Lari-Maca area (Central Andes; southern Peru). A complex, multi-phase development of these structures was revealed. The results show that the structural framework of the Rio Colca valley consists of WNW-ESE and NE-SW faults, and a few W-E faults. The strike of the most common fault sets is approximately parallel (longitudinal) or perpendicular (transverse) to the W-E oriented strike of stratification surfaces in the Mesozoic sedimentary series and the W-E fold macro-structures, developed in these strata. Diagonal faults and joints are less common, allhough at some localities they are numerous. The recurrence of maj or fault syslems throughout the Mesozoic and Miocene series and the Pleislocene-Holocene (mainly colluvial) deposits is proof of recent, tectonic activity in the study area. The recent faulting has led to the development of a syslem of distinct, primary fault scarps, tectonic grabens and horsts, as well as open fissures, which are well marked in the surface morphology, and in many cases have not yet been eroded.},
note = {13},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The network of faults andjoints within the Mesozoic, Miocene and Pleistocene-Holocene formations was studied in the Rio Colca valley, in the Pinchollo-Lari-Maca area (Central Andes; southern Peru). A complex, multi-phase development of these structures was revealed. The results show that the structural framework of the Rio Colca valley consists of WNW-ESE and NE-SW faults, and a few W-E faults. The strike of the most common fault sets is approximately parallel (longitudinal) or perpendicular (transverse) to the W-E oriented strike of stratification surfaces in the Mesozoic sedimentary series and the W-E fold macro-structures, developed in these strata. Diagonal faults and joints are less common, allhough at some localities they are numerous. The recurrence of maj or fault syslems throughout the Mesozoic and Miocene series and the Pleislocene-Holocene (mainly colluvial) deposits is proof of recent, tectonic activity in the study area. The recent faulting has led to the development of a syslem of distinct, primary fault scarps, tectonic grabens and horsts, as well as open fissures, which are well marked in the surface morphology, and in many cases have not yet been eroded.
Malczewski, D.; Żaba, J.
Natural radioactivity in rocks of the Modane-Aussois region (SE France) Journal Article
In: Journal of Radioanalytical and Nuclear Chemistry, vol. 292, no. 1, pp. 123-130, 2012, ISSN: 02365731, (5).
@article{2-s2.0-84858016271,
title = {Natural radioactivity in rocks of the Modane-Aussois region (SE France)},
author = { D. Malczewski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84858016271&doi=10.1007%2fs10967-011-1428-9&partnerID=40&md5=73bf074ad30e900d2a1a3de3493b5924},
doi = {10.1007/s10967-011-1428-9},
issn = {02365731},
year = {2012},
date = {2012-01-01},
journal = {Journal of Radioanalytical and Nuclear Chemistry},
volume = {292},
number = {1},
pages = {123-130},
publisher = {Kluwer Academic Publishers},
abstract = {The activity concentrations of 40 K, 232 Th, and 238 U in the characteristic rocks of the Modane-Aussois region (Western Alps; France) were determined using an HPGe gamma-ray spectrometry system. The activity concentrations of 40 K varied from 18 Bqkg -1 (limestone dolomite) to 392 Bqkg -1 (calcschist), while those of 232 Th varied from 0.7 Bqkg -1 (limestone dolomite) to 18 Bqkg -1 (calcschist). The activities associated with 238 U ranged from 9 (quartzite) to 29 Bqkg -1 (dolomite). In the investigated rock samples, concentrations of 238 U (ppm) and 40 K (%) had a strong negative correlation. © 2011 The Author(s).},
note = {5},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The activity concentrations of 40 K, 232 Th, and 238 U in the characteristic rocks of the Modane-Aussois region (Western Alps; France) were determined using an HPGe gamma-ray spectrometry system. The activity concentrations of 40 K varied from 18 Bqkg -1 (limestone dolomite) to 392 Bqkg -1 (calcschist), while those of 232 Th varied from 0.7 Bqkg -1 (limestone dolomite) to 18 Bqkg -1 (calcschist). The activities associated with 238 U ranged from 9 (quartzite) to 29 Bqkg -1 (dolomite). In the investigated rock samples, concentrations of 238 U (ppm) and 40 K (%) had a strong negative correlation. © 2011 The Author(s).
2010
Słaby, E.; Breitkreuz, C.; Żaba, J.; Domańska-Siuda, J.; Gaidzik, K.; Falenty, K.; Falenty, A.
Magma generation in an alternating transtensional-transpressional regime, the Kraków-Lubliniec Fault Zone, Poland Journal Article
In: Lithos, vol. 119, no. 3-4, pp. 251-268, 2010, ISSN: 00244937, (25).
@article{2-s2.0-77956942574,
title = {Magma generation in an alternating transtensional-transpressional regime, the Kraków-Lubliniec Fault Zone, Poland},
author = { E. Słaby and C. Breitkreuz and J. Żaba and J. Domańska-Siuda and K. Gaidzik and K. Falenty and A. Falenty},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-77956942574&doi=10.1016%2fj.lithos.2010.07.003&partnerID=40&md5=9f65ecdbe1837ea3f4540959e85386fd},
doi = {10.1016/j.lithos.2010.07.003},
issn = {00244937},
year = {2010},
date = {2010-01-01},
journal = {Lithos},
volume = {119},
number = {3-4},
pages = {251-268},
abstract = {In the Kraków-Lubliniec Fault Zone (KLFZ) late Carbonifereous-Permian volcanic rocks mark the boundary between the Małopolska Block (thinned marginal sector of Baltica) and the Upper Silesian Block (a sector of the Brunovistulia composite Terrane). The Zone is a part of the major Hamburg-Kraków-Dobrogea transcontinental strike-slip tectonic zone separating the Laurussian craton and Gondwana blocks which came together to form it. The geochemistry of the volcanic rocks reflects the collisional nature of the tectonism. However, it also presents a signature compatible with extensional magmatism. The paper presents models of magma generation and evolution in what was a zone of alternating transpression and transtension. The magmatism in this zone of amalgamated terranes was related to two different sources: enriched mantle and primitive crust. The lithospheric mantle beneath some blocks of the amalgamated terranes may have experienced enrichment processes during previous subduction events. The metasomatism may have also occurred as a result of crustal thickening during transpression followed by delamination, subsidence and melting. These metasomatised blocks reacted with decompressional melting. Our results show that magma generation and evolution in the zone seem to be not typical examples of late Carbonifereous-Permian magmatism, which is known from other locations throughout Central Europe. © 2010 Elsevier B.V.},
note = {25},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
In the Kraków-Lubliniec Fault Zone (KLFZ) late Carbonifereous-Permian volcanic rocks mark the boundary between the Małopolska Block (thinned marginal sector of Baltica) and the Upper Silesian Block (a sector of the Brunovistulia composite Terrane). The Zone is a part of the major Hamburg-Kraków-Dobrogea transcontinental strike-slip tectonic zone separating the Laurussian craton and Gondwana blocks which came together to form it. The geochemistry of the volcanic rocks reflects the collisional nature of the tectonism. However, it also presents a signature compatible with extensional magmatism. The paper presents models of magma generation and evolution in what was a zone of alternating transpression and transtension. The magmatism in this zone of amalgamated terranes was related to two different sources: enriched mantle and primitive crust. The lithospheric mantle beneath some blocks of the amalgamated terranes may have experienced enrichment processes during previous subduction events. The metasomatism may have also occurred as a result of crustal thickening during transpression followed by delamination, subsidence and melting. These metasomatised blocks reacted with decompressional melting. Our results show that magma generation and evolution in the zone seem to be not typical examples of late Carbonifereous-Permian magmatism, which is known from other locations throughout Central Europe. © 2010 Elsevier B.V.
2009
Zelaźniewicz, A.; Buła, Z.; Fanning, M.; Seghedi, A.; Żaba, J.
More evidence on Neoproterozoic terranes in Southern Poland and southeastern Romania Journal Article
In: Geological Quarterly, vol. 53, no. 1, pp. 93-124, 2009, ISSN: 16417291, (93).
@article{2-s2.0-68949199486,
title = {More evidence on Neoproterozoic terranes in Southern Poland and southeastern Romania},
author = { A. Zelaźniewicz and Z. Buła and M. Fanning and A. Seghedi and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-68949199486&partnerID=40&md5=f7feb5c583f168550815e071e9c6a99a},
issn = {16417291},
year = {2009},
date = {2009-01-01},
journal = {Geological Quarterly},
volume = {53},
number = {1},
pages = {93-124},
abstract = {New geological, geochemical and U-Pb SHRIMP zirconage data brought more information about basement units in subsurface of Southern Poland and SE Romania, which allows to revise and refine some earlier models in the framework of the break-up of the Rodinia/Pannotia supercontinent. In the Brno Block, Moravia, and in the Upper Silesia Block, three different terranes formed the composite Brunovistulia Terrane. The Thaya Terrane (low eNd (T)) of Gondwana (Amazonia) descent collided obliquely at 640-620 Ma with the Slavkov Terrane (moderate eNd (T)) composed of amphibolitefacies metasediments and arc-related, mostly unfoliated granitoids which intruded at 580-560 Ma. At that time, back-arc rifting separated the couple Thaya-Slavkov (inherited zircons: 1.01-1.2; 1.4-1.5; 1.65-1.8 Ga) that drifted away from Gondwana until collision around 560-550 Ma with the Rzeszotary Terrane, the Palaeoproterozoic (2.7-2.0 Ga) crustal sliver deriVěd from Amazonia or West Africa. Atleast these three units composed Brunovistulia, which occurred at low latitudes in proximity to Baltica as shown by palaeomagnetic and palaeobiogeographic data. Then Brunovistulia was accreted to the thinned passive margin of Baltica around its Małopolska promontory/proximal terrane. A complex foreland flysch basin developed in front of the SlavkovRzeszotary suture and across the Rzeszotary-Baltica/Małopolska border. The further from the suture the less amount of the 640-550 Ma detritalzircons extracted from the Thaya-Slavkov hinter land and the smaller eNd (T) values. In West Małopolska, the flysch contains mainly Neoproterozoiczircons (720-550 Ma), whereas in East Małopolska 1.8-2.1 Ga and 2.5 Gazircons dominate, which resembles nearby Baltica. The basin infill was multiphase folded and sheared; in Upper Silesia prior to deposition of the pre-Holmia Cambrian over step. In Małopolska, the folded flysch series formed a large-scale antiformal stack with thermal anticline in its core marked by low-grade metamorphic over print. In Central Dobrogea, Moesia, Ediacaran flysch also contains mainly 700-575 Ma detritalzircons which link the source area, likely in South Dobrogea with ca. 560 Ma granitoids, rather close with Gondwana. However, fauna in Lower Cambrian over step strata shows Baltican affinity. Such features resemble Upper Silesia, thus Brunovistulia might have extended beeath the Carpathians down to Moesia. The other part of South Dobrogea with Palaeoproterozoic iron stones resembles Ukrainian banded iron formation. If true, the Baltican sliver would be incorporated in Moesia. Such a possibility concurs with the provenance data from Ediacaran flysch of Central Dobrogea, which points to up lifted continental block as a source of detrital material. Our study supports an earlier proposition that at the end of the Neoproterozoic a group of small terranes that included Brunovistulia, Moesia and Małopolska formed the Teisseyre-Tornquist Terrane Assemblage (TTA). In our model, a characteristic feature of the TTA was a mixture of crustal elements that were deriVěd from both Gondwana and Baltica, which gave rise to mutual collisions of the elements prior to and concurrent with the docking to Baltica in latest Ediacaran times. The presence of extensive younger covers and complex Phanerozoic evolution of individual members of the TTA impede the recognition of their Neoproterozoic history.},
note = {93},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
New geological, geochemical and U-Pb SHRIMP zirconage data brought more information about basement units in subsurface of Southern Poland and SE Romania, which allows to revise and refine some earlier models in the framework of the break-up of the Rodinia/Pannotia supercontinent. In the Brno Block, Moravia, and in the Upper Silesia Block, three different terranes formed the composite Brunovistulia Terrane. The Thaya Terrane (low eNd (T)) of Gondwana (Amazonia) descent collided obliquely at 640-620 Ma with the Slavkov Terrane (moderate eNd (T)) composed of amphibolitefacies metasediments and arc-related, mostly unfoliated granitoids which intruded at 580-560 Ma. At that time, back-arc rifting separated the couple Thaya-Slavkov (inherited zircons: 1.01-1.2; 1.4-1.5; 1.65-1.8 Ga) that drifted away from Gondwana until collision around 560-550 Ma with the Rzeszotary Terrane, the Palaeoproterozoic (2.7-2.0 Ga) crustal sliver deriVěd from Amazonia or West Africa. Atleast these three units composed Brunovistulia, which occurred at low latitudes in proximity to Baltica as shown by palaeomagnetic and palaeobiogeographic data. Then Brunovistulia was accreted to the thinned passive margin of Baltica around its Małopolska promontory/proximal terrane. A complex foreland flysch basin developed in front of the SlavkovRzeszotary suture and across the Rzeszotary-Baltica/Małopolska border. The further from the suture the less amount of the 640-550 Ma detritalzircons extracted from the Thaya-Slavkov hinter land and the smaller eNd (T) values. In West Małopolska, the flysch contains mainly Neoproterozoiczircons (720-550 Ma), whereas in East Małopolska 1.8-2.1 Ga and 2.5 Gazircons dominate, which resembles nearby Baltica. The basin infill was multiphase folded and sheared; in Upper Silesia prior to deposition of the pre-Holmia Cambrian over step. In Małopolska, the folded flysch series formed a large-scale antiformal stack with thermal anticline in its core marked by low-grade metamorphic over print. In Central Dobrogea, Moesia, Ediacaran flysch also contains mainly 700-575 Ma detritalzircons which link the source area, likely in South Dobrogea with ca. 560 Ma granitoids, rather close with Gondwana. However, fauna in Lower Cambrian over step strata shows Baltican affinity. Such features resemble Upper Silesia, thus Brunovistulia might have extended beeath the Carpathians down to Moesia. The other part of South Dobrogea with Palaeoproterozoic iron stones resembles Ukrainian banded iron formation. If true, the Baltican sliver would be incorporated in Moesia. Such a possibility concurs with the provenance data from Ediacaran flysch of Central Dobrogea, which points to up lifted continental block as a source of detrital material. Our study supports an earlier proposition that at the end of the Neoproterozoic a group of small terranes that included Brunovistulia, Moesia and Małopolska formed the Teisseyre-Tornquist Terrane Assemblage (TTA). In our model, a characteristic feature of the TTA was a mixture of crustal elements that were deriVěd from both Gondwana and Baltica, which gave rise to mutual collisions of the elements prior to and concurrent with the docking to Baltica in latest Ediacaran times. The presence of extensive younger covers and complex Phanerozoic evolution of individual members of the TTA impede the recognition of their Neoproterozoic history.
2008
Buła, Z.; Żaba, J.; Habryn, R.
In: Przeglad Geologiczny, vol. 56, no. 10, pp. 912-920, 2008, ISSN: 00332151, (47).
@article{2-s2.0-58149509615,
title = {Tectonic subdivision of Poland: Southern Poland (Upper Silesian Block, and Małopolska Block) [Regionalizacja tektoniczna Polski - Polska południowa (blok górnoślaski i blok małopolski)]},
author = { Z. Buła and J. Żaba and R. Habryn},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-58149509615&partnerID=40&md5=01a6976999c1d19a0c5f5a8be3ad34a7},
issn = {00332151},
year = {2008},
date = {2008-01-01},
journal = {Przeglad Geologiczny},
volume = {56},
number = {10},
pages = {912-920},
abstract = {The attempt to divide the Upper Silesian Block and the Małopolska Block into tectonic units has been based on a general map at scale of 1:1000000, without Permian-Mesozoic and Cenozoic strata. Cartographic, general and monographic works regarding formation of Precambrian basement of both of the blocks have been discussed and presented, and data concerning development of sedimentation, tectonics, and structure of the Paleozoic cover of the blocks were the background for the suggested division. The Upper Silesian Block is a part of a larger unit determined as the Brunovistulicum, which together with the Brno Block are entirely located within the borders of the Czech Republic. The Brunovistulicum and the Małopolska Block vary information of Precambrian basement and covering Paleozoic formations, what proves different paleogeographical-facial and paleotectonic development. Current data do not allow determining their southern range, where both units are within the range of the orogeny of the Outer Carpathians and quite possibly in the range of the Inner Carpathians. The boundary of the Brunovistulicum and the Małopolska Block along the part between Lubliniec and Cracow and farther to the vicinity of Bochnia and Nowy Sacz is relatively well defined and documented. It is a narrow Cracow-Lubliniec fault zone, approximately 500 m wide, cutting and moving all rock series of the Precambrian and the Paleozoic. The fault zone of the Odra River probably forms its NW continuation. The following tectonic units have been distinguished in the Upper Silesian Block: 1) Moravian-Silesian Fold-and-Thrust Belt, 2) Upper Silesian Fold Zone, 3) Upper Silesian Trough, 4) Bielsko-Biała Dome, 5) Rzeszotary Horst, 6) Liplas Graben. There is only one tectonic unit distinguished in the Małopolska Block - Kielce Fold Belt, dipping towards NW-SE, along the NE boundary of the block. Paleozoic formations building the unit represent thrust fault structure. In this case, the Kielce Fold Belt significantly varies from the other parts of the Małopolska Block, where Paleozoic formations build numerous small block structures.},
note = {47},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The attempt to divide the Upper Silesian Block and the Małopolska Block into tectonic units has been based on a general map at scale of 1:1000000, without Permian-Mesozoic and Cenozoic strata. Cartographic, general and monographic works regarding formation of Precambrian basement of both of the blocks have been discussed and presented, and data concerning development of sedimentation, tectonics, and structure of the Paleozoic cover of the blocks were the background for the suggested division. The Upper Silesian Block is a part of a larger unit determined as the Brunovistulicum, which together with the Brno Block are entirely located within the borders of the Czech Republic. The Brunovistulicum and the Małopolska Block vary information of Precambrian basement and covering Paleozoic formations, what proves different paleogeographical-facial and paleotectonic development. Current data do not allow determining their southern range, where both units are within the range of the orogeny of the Outer Carpathians and quite possibly in the range of the Inner Carpathians. The boundary of the Brunovistulicum and the Małopolska Block along the part between Lubliniec and Cracow and farther to the vicinity of Bochnia and Nowy Sacz is relatively well defined and documented. It is a narrow Cracow-Lubliniec fault zone, approximately 500 m wide, cutting and moving all rock series of the Precambrian and the Paleozoic. The fault zone of the Odra River probably forms its NW continuation. The following tectonic units have been distinguished in the Upper Silesian Block: 1) Moravian-Silesian Fold-and-Thrust Belt, 2) Upper Silesian Fold Zone, 3) Upper Silesian Trough, 4) Bielsko-Biała Dome, 5) Rzeszotary Horst, 6) Liplas Graben. There is only one tectonic unit distinguished in the Małopolska Block - Kielce Fold Belt, dipping towards NW-SE, along the NE boundary of the block. Paleozoic formations building the unit represent thrust fault structure. In this case, the Kielce Fold Belt significantly varies from the other parts of the Małopolska Block, where Paleozoic formations build numerous small block structures.
Buła, Z.; Żaba, J.
In: Przeglad Geologiczny, vol. 56, no. 6, pp. 473-480, 2008, ISSN: 00332151, (23).
@article{2-s2.0-46649120723,
title = {Structure of the Precambrian basement of the eastern part of the Upper Silesia block (Brunovistulicum) [Struktura prekambryjskeigo podłoża wschodniej cześci bloku górnoślaskiego (Brunovistulicum)]},
author = { Z. Buła and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-46649120723&partnerID=40&md5=0b72098d8c1c842c07da8a492fd89a39},
issn = {00332151},
year = {2008},
date = {2008-01-01},
journal = {Przeglad Geologiczny},
volume = {56},
number = {6},
pages = {473-480},
abstract = {Two large, regional tectonic units, represented by Malopolska and Brunovistulicum blocks (terrains) can be distinguished in the southern Poland. The Cracow-Lubliniec fault zone forms their border. They vary both in the structures of the Precambrian basement and the Paleozoic rock cover, which shows different paleogeographic-facies and paleotectonic development. They are separated from the neighboring tectonic units by immense deep fault zones. Archean and Early Proterozoic metamorphic rocks within the Rzeszotary horst (2.6-2.8 and 2.0 Ga) are the oldest formations building the Brunovistulicum basement. Farther to the west, Precambrian and Ediacaran anchimetamorphic siliclastics can be observed. Cadomian-Precambrian rocks (640-545Ma), which outcrop only near Brno, occur south and west of them. In the western part of the Brunovisitulicum (the Western Sudetes) Variscan orthogneiss occurs. The age of its protholite varies vastly; from approximately 1020 Ma through 680-570 Ma to approximately 520-500 Ma. Precambrian basement of the Brunovistulicum is heterogenic. Within the area of Poland, it is formed by two fragments of the crust, represented by Karelian and Early Karelian rocks of the Rzeszotary horst and Cadomian crystalline and anchimetamorphic rocks occurring west of Rzeszotary. Between them, two vast, connected together magnetic maxima in the vicinity of Tychy and Jordanów can be observed in a magnetic field image ΔZ. The origin of those anomalies is related to the occurrence of gabbro, diabase and/or ultrabasite (ophiolite) rocks. Referring to the earlier concepts, it may be currently assumed that the anomaly axis Tychy-Jordanów determines the course of the contact zone (ophiolite suture zone) between the two fragments of the crust of different ages, building the basement of Brunovistulicum: the Archean - Lower Proterozoic (Karelian) and the Upper Proterozoic (Cadomian) formations.},
note = {23},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Two large, regional tectonic units, represented by Malopolska and Brunovistulicum blocks (terrains) can be distinguished in the southern Poland. The Cracow-Lubliniec fault zone forms their border. They vary both in the structures of the Precambrian basement and the Paleozoic rock cover, which shows different paleogeographic-facies and paleotectonic development. They are separated from the neighboring tectonic units by immense deep fault zones. Archean and Early Proterozoic metamorphic rocks within the Rzeszotary horst (2.6-2.8 and 2.0 Ga) are the oldest formations building the Brunovistulicum basement. Farther to the west, Precambrian and Ediacaran anchimetamorphic siliclastics can be observed. Cadomian-Precambrian rocks (640-545Ma), which outcrop only near Brno, occur south and west of them. In the western part of the Brunovisitulicum (the Western Sudetes) Variscan orthogneiss occurs. The age of its protholite varies vastly; from approximately 1020 Ma through 680-570 Ma to approximately 520-500 Ma. Precambrian basement of the Brunovistulicum is heterogenic. Within the area of Poland, it is formed by two fragments of the crust, represented by Karelian and Early Karelian rocks of the Rzeszotary horst and Cadomian crystalline and anchimetamorphic rocks occurring west of Rzeszotary. Between them, two vast, connected together magnetic maxima in the vicinity of Tychy and Jordanów can be observed in a magnetic field image ΔZ. The origin of those anomalies is related to the occurrence of gabbro, diabase and/or ultrabasite (ophiolite) rocks. Referring to the earlier concepts, it may be currently assumed that the anomaly axis Tychy-Jordanów determines the course of the contact zone (ophiolite suture zone) between the two fragments of the crust of different ages, building the basement of Brunovistulicum: the Archean - Lower Proterozoic (Karelian) and the Upper Proterozoic (Cadomian) formations.
Żaba, J.
In: Przeglad Geologiczny, vol. 56, no. 4, pp. 313-314, 2008, ISSN: 00332151.
@article{2-s2.0-46649115913,
title = {Canaima National Park (Guyana Upland, Venezuela) - Geological impressions [Park Narodowy Canaima (Wyżyna Gujańska, Wenezuela ) - Impresje geologiczne]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-46649115913&partnerID=40&md5=cc52ea83eaa9db1fc042e56a303619aa},
issn = {00332151},
year = {2008},
date = {2008-01-01},
journal = {Przeglad Geologiczny},
volume = {56},
number = {4},
pages = {313-314},
abstract = {[No abstract available]},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
Linnemann, U.; Romer, R. L.; Christian, P.; Aleksandrowski, P.; Buła, Z.; Geisler, T.; Kachlik, V.; Krzemińska, E.; Mazur, S.; Motuza, G.; Murphy, J. B.; Nance, R. D.; Pisarevsky, S. A.; Schulz, B.; Ulrich, J.; Wiszniewska, J.; Żaba, J.; Armin, Z.
Precambrian Journal Article
In: Central Europe, vol. 1, pp. 21-101, 2008, ISSN: 14790963, (34).
@article{2-s2.0-61149513465,
title = {Precambrian},
author = { U. Linnemann and R.L. Romer and P. Christian and P. Aleksandrowski and Z. Buła and T. Geisler and V. Kachlik and E. Krzemińska and S. Mazur and G. Motuza and J.B. Murphy and R.D. Nance and S.A. Pisarevsky and B. Schulz and J. Ulrich and J. Wiszniewska and J. Żaba and Z. Armin},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-61149513465&doi=10.1144%2fcev1p.2&partnerID=40&md5=805a1a270c8804414686bd6a2728fd1c},
doi = {10.1144/cev1p.2},
issn = {14790963},
year = {2008},
date = {2008-01-01},
journal = {Central Europe},
volume = {1},
pages = {21-101},
publisher = {Maney Publishing},
abstract = {The Precambian of Central Europe and adjoining areas belongs to two principal geotectonic domains represented by (1) Baltica that forms a part of the East European Craton (EEC), and (2) peri-Gondwana. Both parts are separated by the Trans-European Suture Zone which is the boundary between the ancient Precambrian lithosphere of the craton and the younger lithosphere beneath the late Neoproterozoic and Palaeozoic peri-Gondwanan mobile belts of Central and western Europe. The peri-Gondwanan units of Central Europe are situated SW of the suture and subdivided into Avalonia and Cadomia, separated by the Rheic Ocean suture. The Baltica part of the EEC consists of three major blocks, namely, Fennoscandia, Sarmatia and Volga - Ural which are characterized by different structures and evolution over a period extending from the Archaean to Palaeoproterozoic. Palaeomagnetic data reveal that Fennoscandia and Sarmatia were separate until c. 1.85 Ga, i.e. until the time of their amalgamation into Baltica. It is assumed that Fennoscandia comprises a mosaic of several Archaean blocks surrounded by accreted crust, generally younging westwards, i.e. in the direction of the Trans-European Suture Zone. These younger orogenic belts include the c. 1.95-1.82 Ga Svecofennian Domain, the c. 1.80-1.65 Ga Trans-Scandinavian Igneous Belt, and a series of 1.75-1.55 Ga magmatic arcs that were variably overprinted during the 1.04-0.97 Ga Sveconorwegian Orogeny. A recent tectonic model suggests the presence of Svecofennian terranes extending across the Baltic and into the Black Sea area. AU parts of Baltica in Central Europe and adjoining areas belong to Fennoscandia (southern Sweden; NE Poland; Lithuania; parts of the basement in the Baltic Sea). Avalonia is a microcontinent or terrane derived from the periphery of West Gondwana. The Neoproterozoic basement of Avalonia formed during Avalonian orogenic processes and related tectonomagmatic events (c. 750-540 Ma). Neoproterozoic and Early Palaeozoic sediments of Avalonia contain detrital zircon grains of Mesoproterozoic age, which are assumed to have formed in a juvenile crust between 1.0 and 1.3 Ga. There is evidence that a large part of Avalonia originated at the margin of Amazonia. Avalonia rifted off from the Gondwanan margin in the late Cambrian/early Ordovician. The Rheic Ocean opened as the Tornquist Sea closed due to the collision of Avalonia with Baltica during the late Ordovician and the early Silurian. In the late Silurian, Baltica plus Avalonia collided with Laurentia coincident with the closure of the Iapetus Ocean to form the short-lived continent of Laurussia. During its drift, and following amalgamation with Baltica and Laurentia, Avalonia represented the northern margin of the Rheic Ocean. Avalonia forms the poorly exposed basement of the Rhenohercynian Zone, extending from the Brabant Massif of Belgium to the eastern margin of the Bohemian Massif. The most important parts of East Avalonia are located in southern Britain and Ireland. Other more easterly parts of Avalonia and related terranes, as well as terranes of uncertain origin along the recent SW margin of Baltica, are summarized as Far East Avalonia. In this chapter, we include the Eckergneiss Complex in the Harz Mountains (Rhenohercynian Zone), the Upper Silesian and Malopolska blocks (SE Poland) and the Thaya and Slavkov terranes, including the so-called Metabasite Belt (eastern Bohemia), as parts of Far East Avalonia. Cadomia is a belt of Neoproterozoic rock units formed by Cadomian orogenic processes at an active margin at the periphery of the West African Craton of Gondwana. Rock units of Cadomia show few or no zircon grains with ages in the range 0.75-1.6 Ga and are dominated by detritus from the West African Craton (2.05 Ga and older). A c. 2.0 Ga crust was recycled. Basement slivers of c. 2 Ga rocks such as the Icartian basement occur locally. The Cadomian basement was formed by Cadomian orogenic processes (c. 750-530 Ma). It includes Neoproterozoic volcanosedimentary complexes and intrusions and early Cambrian (c. 540-530 Ma) plutons intruded during a final intense tectonothermal event. Most probably, Cadomia never left the Gondwana mainland and did not drift off like Avalonia. During the assemblage of the Pangaea Supercontinent by Variscan orogenic events, the Rheic Ocean closed as a result of the continent-continent collision between Laurussia and Gondwana in Late Devonian-Early Carboniferous times. The Mid-German Crystalline Zone at the northern rim of the Bohemian Massif is believed to represent the suture of the Rheic Ocean. The suture was formed by oblique collision between the Bohemian (Cadomia; Gondwana) and Rhenish massifs (Avalonia; Laurussia) in Variscan times during the Late Devonian to Early Carboniferous. During its origin Neoproterozoic crust became recyled and parts of Cadomia and Avalonia amalgamated. Cadomia includes the Armorican Massif, Pyrénées, French Massif Central, Maures Massif, Corsica, and the largest part of the Bohemian Massif such as the Saxo-Thuringian Zone, the Sudetes, and the Moldanubian Zone. The latter contains the Teplä-Barrandian Unit and the Moldanubicum sensu stricto. The oldest units of the Bohemian Massif are remnants of Palaeo- to Mesoproterozoic cratonic basement slivers such as the Dobra gneiss (1.38 Ga) and the Svetlik gneiss (2.05-2.1 Ga). Parts of the Bohemian Massif are related to Far East Avalonia such as the Brunovistulian Block of the Moravo-Silesian Zone (eastern Bohemia) and the Upper Silesian and Malopolska blocks (SE Poland). It is likely that the peri-Gondwanan basement of the Alps also was a part of Cadomia although the occurrence of Mesoproterozoic zircon points to the possibility of an origin west of the West African Craton.},
note = {34},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Precambian of Central Europe and adjoining areas belongs to two principal geotectonic domains represented by (1) Baltica that forms a part of the East European Craton (EEC), and (2) peri-Gondwana. Both parts are separated by the Trans-European Suture Zone which is the boundary between the ancient Precambrian lithosphere of the craton and the younger lithosphere beneath the late Neoproterozoic and Palaeozoic peri-Gondwanan mobile belts of Central and western Europe. The peri-Gondwanan units of Central Europe are situated SW of the suture and subdivided into Avalonia and Cadomia, separated by the Rheic Ocean suture. The Baltica part of the EEC consists of three major blocks, namely, Fennoscandia, Sarmatia and Volga - Ural which are characterized by different structures and evolution over a period extending from the Archaean to Palaeoproterozoic. Palaeomagnetic data reveal that Fennoscandia and Sarmatia were separate until c. 1.85 Ga, i.e. until the time of their amalgamation into Baltica. It is assumed that Fennoscandia comprises a mosaic of several Archaean blocks surrounded by accreted crust, generally younging westwards, i.e. in the direction of the Trans-European Suture Zone. These younger orogenic belts include the c. 1.95-1.82 Ga Svecofennian Domain, the c. 1.80-1.65 Ga Trans-Scandinavian Igneous Belt, and a series of 1.75-1.55 Ga magmatic arcs that were variably overprinted during the 1.04-0.97 Ga Sveconorwegian Orogeny. A recent tectonic model suggests the presence of Svecofennian terranes extending across the Baltic and into the Black Sea area. AU parts of Baltica in Central Europe and adjoining areas belong to Fennoscandia (southern Sweden; NE Poland; Lithuania; parts of the basement in the Baltic Sea). Avalonia is a microcontinent or terrane derived from the periphery of West Gondwana. The Neoproterozoic basement of Avalonia formed during Avalonian orogenic processes and related tectonomagmatic events (c. 750-540 Ma). Neoproterozoic and Early Palaeozoic sediments of Avalonia contain detrital zircon grains of Mesoproterozoic age, which are assumed to have formed in a juvenile crust between 1.0 and 1.3 Ga. There is evidence that a large part of Avalonia originated at the margin of Amazonia. Avalonia rifted off from the Gondwanan margin in the late Cambrian/early Ordovician. The Rheic Ocean opened as the Tornquist Sea closed due to the collision of Avalonia with Baltica during the late Ordovician and the early Silurian. In the late Silurian, Baltica plus Avalonia collided with Laurentia coincident with the closure of the Iapetus Ocean to form the short-lived continent of Laurussia. During its drift, and following amalgamation with Baltica and Laurentia, Avalonia represented the northern margin of the Rheic Ocean. Avalonia forms the poorly exposed basement of the Rhenohercynian Zone, extending from the Brabant Massif of Belgium to the eastern margin of the Bohemian Massif. The most important parts of East Avalonia are located in southern Britain and Ireland. Other more easterly parts of Avalonia and related terranes, as well as terranes of uncertain origin along the recent SW margin of Baltica, are summarized as Far East Avalonia. In this chapter, we include the Eckergneiss Complex in the Harz Mountains (Rhenohercynian Zone), the Upper Silesian and Malopolska blocks (SE Poland) and the Thaya and Slavkov terranes, including the so-called Metabasite Belt (eastern Bohemia), as parts of Far East Avalonia. Cadomia is a belt of Neoproterozoic rock units formed by Cadomian orogenic processes at an active margin at the periphery of the West African Craton of Gondwana. Rock units of Cadomia show few or no zircon grains with ages in the range 0.75-1.6 Ga and are dominated by detritus from the West African Craton (2.05 Ga and older). A c. 2.0 Ga crust was recycled. Basement slivers of c. 2 Ga rocks such as the Icartian basement occur locally. The Cadomian basement was formed by Cadomian orogenic processes (c. 750-530 Ma). It includes Neoproterozoic volcanosedimentary complexes and intrusions and early Cambrian (c. 540-530 Ma) plutons intruded during a final intense tectonothermal event. Most probably, Cadomia never left the Gondwana mainland and did not drift off like Avalonia. During the assemblage of the Pangaea Supercontinent by Variscan orogenic events, the Rheic Ocean closed as a result of the continent-continent collision between Laurussia and Gondwana in Late Devonian-Early Carboniferous times. The Mid-German Crystalline Zone at the northern rim of the Bohemian Massif is believed to represent the suture of the Rheic Ocean. The suture was formed by oblique collision between the Bohemian (Cadomia; Gondwana) and Rhenish massifs (Avalonia; Laurussia) in Variscan times during the Late Devonian to Early Carboniferous. During its origin Neoproterozoic crust became recyled and parts of Cadomia and Avalonia amalgamated. Cadomia includes the Armorican Massif, Pyrénées, French Massif Central, Maures Massif, Corsica, and the largest part of the Bohemian Massif such as the Saxo-Thuringian Zone, the Sudetes, and the Moldanubian Zone. The latter contains the Teplä-Barrandian Unit and the Moldanubicum sensu stricto. The oldest units of the Bohemian Massif are remnants of Palaeo- to Mesoproterozoic cratonic basement slivers such as the Dobra gneiss (1.38 Ga) and the Svetlik gneiss (2.05-2.1 Ga). Parts of the Bohemian Massif are related to Far East Avalonia such as the Brunovistulian Block of the Moravo-Silesian Zone (eastern Bohemia) and the Upper Silesian and Malopolska blocks (SE Poland). It is likely that the peri-Gondwanan basement of the Alps also was a part of Cadomia although the occurrence of Mesoproterozoic zircon points to the possibility of an origin west of the West African Craton.
2007
Malczewski, D.; Żaba, J.
222Rn and 220Rn concentrations in soil gas of Karkonosze-Izera Block (Sudetes, Poland) Journal Article
In: Journal of Environmental Radioactivity, vol. 92, no. 3, pp. 144-164, 2007, ISSN: 0265931X, (11).
@article{2-s2.0-33846504073,
title = {222Rn and 220Rn concentrations in soil gas of Karkonosze-Izera Block (Sudetes, Poland)},
author = { D. Malczewski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-33846504073&doi=10.1016%2fj.jenvrad.2006.11.001&partnerID=40&md5=982e045e60d006c57dfb71f0a5ae1c2f},
doi = {10.1016/j.jenvrad.2006.11.001},
issn = {0265931X},
year = {2007},
date = {2007-01-01},
journal = {Journal of Environmental Radioactivity},
volume = {92},
number = {3},
pages = {144-164},
abstract = {Soil gas 222Rn and 220Rn concentrations were measured at 18 locations in the Karkonosze-Izera Block area in southwestern Poland. Measurements were carried out in surface air and at sampling depths of 10, 40 and 80 cm. Surface air 222Rn concentrations ranged from 4 to 2160 Bq m-3 and 220Rn ranged from 4 to 228 Bq m-3. The concentrations for 10 and 40 cm varied from 142 Bq m-3 to 801 kBq m-3 and 102 Bq m-3 to 64 kBq m-3 for 222Rn and 220Rn, respectively. At 80 cm 222Rn concentrations ranged from 94 Bq m-3 to >1 MBq m-3. The 220Rn concentrations at 80 cm varied from 45 Bq m-3 to 48 kBq m-3. The concentration versus depth profiles for 222Rn differed for soils developed on fault zones, uranium deposits or both. Atmospheric air temperature and soil gas 222Rn and 220Rn were negatively correlated. At sampling sites with steep slopes, 220Rn concentrations decreased with depth. © 2006 Elsevier Ltd. All rights reserved.},
note = {11},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Soil gas 222Rn and 220Rn concentrations were measured at 18 locations in the Karkonosze-Izera Block area in southwestern Poland. Measurements were carried out in surface air and at sampling depths of 10, 40 and 80 cm. Surface air 222Rn concentrations ranged from 4 to 2160 Bq m-3 and 220Rn ranged from 4 to 228 Bq m-3. The concentrations for 10 and 40 cm varied from 142 Bq m-3 to 801 kBq m-3 and 102 Bq m-3 to 64 kBq m-3 for 222Rn and 220Rn, respectively. At 80 cm 222Rn concentrations ranged from 94 Bq m-3 to >1 MBq m-3. The 220Rn concentrations at 80 cm varied from 45 Bq m-3 to 48 kBq m-3. The concentration versus depth profiles for 222Rn differed for soils developed on fault zones, uranium deposits or both. Atmospheric air temperature and soil gas 222Rn and 220Rn were negatively correlated. At sampling sites with steep slopes, 220Rn concentrations decreased with depth. © 2006 Elsevier Ltd. All rights reserved.
2006
Żaba, J.; Poprawa, P.
In: Prace - Panstwowego Instytutu Geologicznego, no. 186, pp. 225-252, 2006, ISSN: 08669465, (8).
@article{2-s2.0-33845372287,
title = {Deformation history of the Koszalin-Chojnice zone (Pomeranian segment of TESZ, NW Poland) constraints from structural analysis of Palaeozoic and Mesozoic successions in Polskie Łaki PIG 1 and Toruń 1 boreholes [Historia deformacji strefy Koszalin-Chojnice (pomorski segment szwu transeuropejskiego) na podstawie analizy strukturalnej utworów paleozoicznych i mezozoicznych w otworach Polskie Łaki PIG 1 i Toruń 1]},
author = { J. Żaba and P. Poprawa},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-33845372287&partnerID=40&md5=c7044569fee13469570816fb419cd099},
issn = {08669465},
year = {2006},
date = {2006-01-01},
journal = {Prace - Panstwowego Instytutu Geologicznego},
number = {186},
pages = {225-252},
abstract = {The recent tectonic structure of the Palaeozoic and Mesozoic successions observed in the Polskie Łaki PIG 1 and Toruń 1 boreholes (the Koszalin-Chojnice zone) was formed as a result of multiphase deformations, related mainly to contractional and transpressional regime, while impact of tectonic processes related to extensional and transtensional regime was less pronounced. The oldest, recognized episodes of deformation were associated with contractional and strike-slip tectonic activity. This led to development of bending-related macro-and mesofolds F1 and cleavage S1, schistosity S2 and recumbent mesofolds F2, as well as schistosity S3 and vertical or steeply dipping mesofolds F3. Sediments involved in this deformation are generally characterized by fold and thrust tectonic style, steep tectonic dipping causing significant angular unconformity with the overlying successions. The latter are also much less affected by diagenesis as compared with successions involved in deformation D1-D3. These deformations could be related to the Caledonian collision of Avalonia and Baltica and to an impact of developing orogen onto tectonic regime of its foreland. Left-lateral component of the deformation D1-D3 probably reflects oblique character of the collision. The deformation D1-D3 developed presumably during the Early Silurian time (Llandovery). Tectonic activity at the end of Silurian-beginning of Devonian was probably of the lesser importance than intra-Silurian one. The following, younger episodes of tectonic activity led to development of deformation revealing very changeable tectonic regime, from extensional and transtensional to transpressional and compressional. This generation of deformations was probably related to Variscan and post-Variscan (pre-late Permian) stage of evolution of the study area, in particular with the late Carboniferous-early Permian significant uplift and fault block tectonics. This stage of deformation led to development of calcite veins, fold structures F4, i.e. broad folds as well as dragged and parasitic folds with lateral or sub-lateral fold axes, zones of mylonitzation and tectonic breccias, sub-vertical normal faults with right-lateral strike-slip component, and broad recumbent folds F5. Moreover, kakirites, cataclasites and, less common, mylonites locally developed at this stage. The next of the main stages of deformation in the Koszalin-Chojnice zone encompassed several episodes related to extensional (transtesional?) and transpressional tectonic regime. This deformation developed probably during the Late Triassic to the late-most Cretaceous-earlymost Cainozoic. The deformation are interpreted as an expression of development of transtensional tectonic grabens in the Late Triassic-Early Jurassic and, to a lesser degree, in the Middle Jurassic and Early Cretaceous, as well as of their subsequent tectonic inversion in the Late Cretaceous and the latemost Cretaceous-earlymost Cainozoic time. This stage of deformation is characterized by development of normal faults, often with right-lateral strike component, calcite veins as well as strike-slip faults and thrust with strike-slip component.},
note = {8},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The recent tectonic structure of the Palaeozoic and Mesozoic successions observed in the Polskie Łaki PIG 1 and Toruń 1 boreholes (the Koszalin-Chojnice zone) was formed as a result of multiphase deformations, related mainly to contractional and transpressional regime, while impact of tectonic processes related to extensional and transtensional regime was less pronounced. The oldest, recognized episodes of deformation were associated with contractional and strike-slip tectonic activity. This led to development of bending-related macro-and mesofolds F1 and cleavage S1, schistosity S2 and recumbent mesofolds F2, as well as schistosity S3 and vertical or steeply dipping mesofolds F3. Sediments involved in this deformation are generally characterized by fold and thrust tectonic style, steep tectonic dipping causing significant angular unconformity with the overlying successions. The latter are also much less affected by diagenesis as compared with successions involved in deformation D1-D3. These deformations could be related to the Caledonian collision of Avalonia and Baltica and to an impact of developing orogen onto tectonic regime of its foreland. Left-lateral component of the deformation D1-D3 probably reflects oblique character of the collision. The deformation D1-D3 developed presumably during the Early Silurian time (Llandovery). Tectonic activity at the end of Silurian-beginning of Devonian was probably of the lesser importance than intra-Silurian one. The following, younger episodes of tectonic activity led to development of deformation revealing very changeable tectonic regime, from extensional and transtensional to transpressional and compressional. This generation of deformations was probably related to Variscan and post-Variscan (pre-late Permian) stage of evolution of the study area, in particular with the late Carboniferous-early Permian significant uplift and fault block tectonics. This stage of deformation led to development of calcite veins, fold structures F4, i.e. broad folds as well as dragged and parasitic folds with lateral or sub-lateral fold axes, zones of mylonitzation and tectonic breccias, sub-vertical normal faults with right-lateral strike-slip component, and broad recumbent folds F5. Moreover, kakirites, cataclasites and, less common, mylonites locally developed at this stage. The next of the main stages of deformation in the Koszalin-Chojnice zone encompassed several episodes related to extensional (transtesional?) and transpressional tectonic regime. This deformation developed probably during the Late Triassic to the late-most Cretaceous-earlymost Cainozoic. The deformation are interpreted as an expression of development of transtensional tectonic grabens in the Late Triassic-Early Jurassic and, to a lesser degree, in the Middle Jurassic and Early Cretaceous, as well as of their subsequent tectonic inversion in the Late Cretaceous and the latemost Cretaceous-earlymost Cainozoic time. This stage of deformation is characterized by development of normal faults, often with right-lateral strike component, calcite veins as well as strike-slip faults and thrust with strike-slip component.
Truszel, M.; Karwowski, Ł.; Lasoń, K.; Markiewicz, J.; Żaba, J.
In: Biuletyn - Panstwowego Instytutu Geologicznego, no. 418, pp. 55-103, 2006, ISSN: 02086603, (14).
@article{2-s2.0-33747198786,
title = {Magmatism and metamorphism of the Kraków-Lubliniec Tectonic zone as a clue to the occurrence of polymetallic deposits [Magmatyzm i metamorfizm strefy tektonicznej Kraków-Lubliniec jako przesłanki wystepowania złóżpolimetalicznych]},
author = { M. Truszel and Ł. Karwowski and K. Lasoń and J. Markiewicz and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-33747198786&partnerID=40&md5=0f2b063385838e87779a3fde21135def},
issn = {02086603},
year = {2006},
date = {2006-01-01},
journal = {Biuletyn - Panstwowego Instytutu Geologicznego},
number = {418},
pages = {55-103},
abstract = {Numerous occurrences of magmatism are observed in the vicinity of Myszków, Zawiercie, Pilica, Bedkowska Valley, Kozieglowy (Myslów) and Żarki along the Kraków-Lubliniec tectonic zone which is a contact zone of the Małopolska and Upper Silesia blocks. The formation of granitoid intrusion is related to a multiphase structural evolution of the zone whose especially intensive activity took place at the end of the Silurian and Upper Carboniferous. Ore mineralization occurs both in igneous and metamorphic wall rocks (Vendian; Palaeozoic). Igneous rocks consist of a genetically different association of intrusive rocks: granitoids (mainly granodiorites; rare granites), dacites, dolerites (diabases) and gabbros. Alterations, which show regional metamorphic nature (greenschist facies), were recorded only in the Vendian complex formations, while thermal and thermal -metasomatic metamorphism, being the effect of influence of granitoid intrusion into wall rocks, affected Vendian, Ordovician, Silurian and Devonian formations. Ore contents of the rocks show direct relationship with highly concentrated metal-rich salinewaters, closely related to acid magmatism. W, Mo, Cu, Ag, K, F, Sb, Hg, Au, Pb, Ba, As, Zn, Bi and Te are elements-pathfinders which can be applied to searching for covered porphyry deposits in other parts of the region.},
note = {14},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Numerous occurrences of magmatism are observed in the vicinity of Myszków, Zawiercie, Pilica, Bedkowska Valley, Kozieglowy (Myslów) and Żarki along the Kraków-Lubliniec tectonic zone which is a contact zone of the Małopolska and Upper Silesia blocks. The formation of granitoid intrusion is related to a multiphase structural evolution of the zone whose especially intensive activity took place at the end of the Silurian and Upper Carboniferous. Ore mineralization occurs both in igneous and metamorphic wall rocks (Vendian; Palaeozoic). Igneous rocks consist of a genetically different association of intrusive rocks: granitoids (mainly granodiorites; rare granites), dacites, dolerites (diabases) and gabbros. Alterations, which show regional metamorphic nature (greenschist facies), were recorded only in the Vendian complex formations, while thermal and thermal -metasomatic metamorphism, being the effect of influence of granitoid intrusion into wall rocks, affected Vendian, Ordovician, Silurian and Devonian formations. Ore contents of the rocks show direct relationship with highly concentrated metal-rich salinewaters, closely related to acid magmatism. W, Mo, Cu, Ag, K, F, Sb, Hg, Au, Pb, Ba, As, Zn, Bi and Te are elements-pathfinders which can be applied to searching for covered porphyry deposits in other parts of the region.
Matyszkiewicz, J.; Krajewski, M.; Żaba, J.
Structural control on the distribution of Upper Jurassic carbonate buildups in the Kraków - Wieluń Upland (South Poland) Journal Article
In: Neues Jahrbuch fur Geologie und Palaontologie - Monatshefte, no. 3, pp. 182-192, 2006, ISSN: 00283630, (24).
@article{2-s2.0-33645821886,
title = {Structural control on the distribution of Upper Jurassic carbonate buildups in the Kraków - Wieluń Upland (South Poland)},
author = { J. Matyszkiewicz and M. Krajewski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-33645821886&doi=10.1127%2fnjgpm%2f2006%2f2006%2f182&partnerID=40&md5=786eb1cb13b3820e02ff369ae8e8f174},
doi = {10.1127/njgpm/2006/2006/182},
issn = {00283630},
year = {2006},
date = {2006-01-01},
journal = {Neues Jahrbuch fur Geologie und Palaontologie - Monatshefte},
number = {3},
pages = {182-192},
publisher = {E. Schweizerbart'sche Verlagsbuchhandlung},
abstract = {The Kraków-Wieluń Upland in southern Poland bears numerous complexes of carbonate buildups which developed in Late Jurassic times upon the stable, northern shelf of the Tethys Ocean. Intensive growth of these structures was strongly controlled by structural properties of their bedrock. The Proterozoic and Palaeozoic bedrock of the Kraków-Wieluń Upland is cut by an important fault zone which separates terrane-like crustal blocks. This zone is accompanied by manifestations of Palaeozoic magmatism, and particularly granitoid plutonism. The location of granitoid batholiths in the basement correlates very well with that of the Upper Jurassic carbonate buildups. Some of the intrusions became probably erosionally exposed in the Early Mesozoic, forming topographic highs upon the Late Jurassic carbonate ramp. The areas underlain by those intrusions whose top parts were not eroded revealed less intense subsidence as compared to the neighbouring regions, thereby creating favourable structural highs upon the sea bottom. Such highs became colonised by benthic organisms, the intense development of which finally led to the growth of carbonate buildups. © 2006 E. Schweizerbart'sche Verlagsbuchhandlung.},
note = {24},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Kraków-Wieluń Upland in southern Poland bears numerous complexes of carbonate buildups which developed in Late Jurassic times upon the stable, northern shelf of the Tethys Ocean. Intensive growth of these structures was strongly controlled by structural properties of their bedrock. The Proterozoic and Palaeozoic bedrock of the Kraków-Wieluń Upland is cut by an important fault zone which separates terrane-like crustal blocks. This zone is accompanied by manifestations of Palaeozoic magmatism, and particularly granitoid plutonism. The location of granitoid batholiths in the basement correlates very well with that of the Upper Jurassic carbonate buildups. Some of the intrusions became probably erosionally exposed in the Early Mesozoic, forming topographic highs upon the Late Jurassic carbonate ramp. The areas underlain by those intrusions whose top parts were not eroded revealed less intense subsidence as compared to the neighbouring regions, thereby creating favourable structural highs upon the sea bottom. Such highs became colonised by benthic organisms, the intense development of which finally led to the growth of carbonate buildups. © 2006 E. Schweizerbart'sche Verlagsbuchhandlung.
2005
Malczewski, D.; Sitarek, A.; Żaba, J.; Dorda, J.
In: Przeglad Geologiczny, vol. 53, no. 3, pp. 237-244, 2005, ISSN: 00332151, (11).
@article{2-s2.0-17344366488,
title = {Natural radioactivity of selected crystalline rocks of the Izera Block (Sudetes, SW Poland) [Promieniotwórczość naturalna wybranych skał krystalicznych bloku izerskiego]},
author = { D. Malczewski and A. Sitarek and J. Żaba and J. Dorda},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-17344366488&partnerID=40&md5=fe5035d50417a0636303765039b33df7},
issn = {00332151},
year = {2005},
date = {2005-01-01},
journal = {Przeglad Geologiczny},
volume = {53},
number = {3},
pages = {237-244},
abstract = {Results of natural radioactivity of 40K, 208Tl, 212Pb, 212Bi, 214Pb, 214Bi, 228Ac and the fallout of 137Cs measured in situ in typical crystalline (both igneous and metamorphic) rocks of the Izera Block (Sudetes Mountains; southwestern Poland) using a portable gamma-ray spectrometry workstation are presented. The highest activity concentrations of 40K and 226Ra (238U series) were noted in laminated gneisses whereas the highest activity concentration of 228Ac (232Th series) is characteristic for Sn-bearing mica schists. The lowest activity concentrations of 40K, 228Ac and 226Ra refer to the basalts, flaser gneisses and Izera granites, respectively. The measurements carried out in the study area have shown relatively low level of 137Cs fallout.},
note = {11},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Results of natural radioactivity of 40K, 208Tl, 212Pb, 212Bi, 214Pb, 214Bi, 228Ac and the fallout of 137Cs measured in situ in typical crystalline (both igneous and metamorphic) rocks of the Izera Block (Sudetes Mountains; southwestern Poland) using a portable gamma-ray spectrometry workstation are presented. The highest activity concentrations of 40K and 226Ra (238U series) were noted in laminated gneisses whereas the highest activity concentration of 228Ac (232Th series) is characteristic for Sn-bearing mica schists. The lowest activity concentrations of 40K, 228Ac and 226Ra refer to the basalts, flaser gneisses and Izera granites, respectively. The measurements carried out in the study area have shown relatively low level of 137Cs fallout.
1999
Żaba, J.
In: Prace - Panstwowego Instytutu Geologicznego, no. 166, pp. X-142, 1999, ISSN: 08669465, (56).
@article{2-s2.0-0002393178,
title = {The structural evolution of lower palaeozoic succession in the Upper Silesia Block and Małopolska Block border zone (Southern Poland) [Ewolucja strukturalna utworów dolnopaleozoicznych w strefie granicznej Bloków Górnośla̧skiego i Małopolskiego]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0002393178&partnerID=40&md5=a2be417d6b24a820f64795f885a47262},
issn = {08669465},
year = {1999},
date = {1999-01-01},
journal = {Prace - Panstwowego Instytutu Geologicznego},
number = {166},
pages = {X-142},
abstract = {[No abstract available]},
note = {56},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
1997
Żaba, J.
In: Prace - Panstwowego Instytutu Geologicznego, no. 157 PART 2, pp. 213-214, 1997, ISSN: 08669465, (3).
@article{2-s2.0-27844478267,
title = {Palaeozoic tectonic activity of the Cracow-Lubliniec (Hamburg-Cracow) fault zone at the boundary of the Upper Silesia and Małopolska blocks, southern Poland},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-27844478267&partnerID=40&md5=020eea917853e578b3ff8ce10be4d4f1},
issn = {08669465},
year = {1997},
date = {1997-01-01},
journal = {Prace - Panstwowego Instytutu Geologicznego},
number = {157 PART 2},
pages = {213-214},
abstract = {[No abstract available]},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
[No abstract available]
Perski, Z.; Żaba, J.
In: Przeglad Geologiczny, vol. 45, no. 1, pp. 51-57, 1997, ISSN: 00332151, (2).
@article{2-s2.0-0039697735,
title = {Structure of the Cambrian and Devonian clastic sediments at Klucze in the Olkusz area (NE edge of the Upper Silesia Block, Southern Poland) [Tektonika klastycznych utworów kambru i dewonu w Kluczach koło Olkusza (NE krawȩdź bloku górnośla̧skiego)]},
author = { Z. Perski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0039697735&partnerID=40&md5=631c2a7b45ea800715af27f7efbf234e},
issn = {00332151},
year = {1997},
date = {1997-01-01},
journal = {Przeglad Geologiczny},
volume = {45},
number = {1},
pages = {51-57},
abstract = {Borehole Klucze 1 is situated in the NE edge zone of the Upper Silesia block, some 9 km to the east from the border with the Małopolska block (fig. 1). The Cracow-Lubliniec fault zone occurs along the border between the Upper Silesian block and the Matopolska block (Buła, 1994). The Cracow-Lubliniec fault zone is a part of the Hamburg-Cracow transcontinental fault zone. Borehole Klucze 1 was located on the SSW wing of the Chechło-Golczowice anticline (figs 1 and 2). Three structural units have been recognized there (figs 2 and 3): 1 - built of Permian, Triassic, Jurassic, and Quaternary rocks; 2 - Variscian which consists of Devonian carbonates and clastic sediments; 3 - Caledonian Lower Cambrian clastic sediments. Distinct angular unconformity occus at the boundary between each of the structural units (figs 2 and 3). The investigated clastic sediments of Lower Cambrian (Buta, 1994; Bute & Jachowicz, 1995) and Lower Devonian (Tarnowska, 1989) consist of intercalated quartz sandstones, and mudstones with subordinate siltstones (Głedysz, 1984) (fig. 3). Structural investigations were also applied to dolomites which crop out in the Stare Gliny quarry (figs 2, 7h). Numerous generations of both sedimentary and tectonic structures have been distinguished in the investigated rocks (figs 4, 5 and 6). They include joint sets (kathetal joints and diagonal joints with features typical of shear joints), strike-slip mesofaults, and normal-slip faults, usually with tectonic breccia (figs 4-7). Fifteen episodes which constitute a geometrical-chronological sequence of different geological events, have been recognized. Based on them 8 stages of structural development of Lower Cambrian and Lower Devonian clastic sediments have been determined. Stage 1 includes sedimentation and diagenesis of Lower Cambrian rocks. Stage 2 was related to minor folding of Lower Cambrian rocks, most probably after early or after Middle Cambrian. Stage 3 involved denudation of Lower Cambrian rocks during late Cambrian, Ordovician and Sylurian. During stage 4 the sedimentation and diagenesis of Devonian rocks occurred. Stage 5 includes folding of both Lower Cambrian and Devonian formations, most probably between Early and Late Carboniferous or even after Namurian A (Oberc, 1993; Bukowy, 1994) under dextral transpresive regime (Żaba, 1994b, 1996). Stage 6 was related to the dextral shearing regime and occurred at the end of Visean (Żaba, 1994b, 1996). During stage 7 the subhorizontal and sinistral strike-slip brittle shear occurred under the sinistral transtensive regime (Żaba, 1994b) from late Carboniferous until early Triassic. The sinistral strike-slip brittle shear was also observed in granites of the edge zone of the Matopolska block (Żaba, 1994a). Stage 8 includes Alpine deformations whitch occurred after the earliest Triassic. Tectonic style of the investigated formations developed predominantly during the stage 5. At that stage the ChechłoGolczowice anticline formed.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Borehole Klucze 1 is situated in the NE edge zone of the Upper Silesia block, some 9 km to the east from the border with the Małopolska block (fig. 1). The Cracow-Lubliniec fault zone occurs along the border between the Upper Silesian block and the Matopolska block (Buła, 1994). The Cracow-Lubliniec fault zone is a part of the Hamburg-Cracow transcontinental fault zone. Borehole Klucze 1 was located on the SSW wing of the Chechło-Golczowice anticline (figs 1 and 2). Three structural units have been recognized there (figs 2 and 3): 1 - built of Permian, Triassic, Jurassic, and Quaternary rocks; 2 - Variscian which consists of Devonian carbonates and clastic sediments; 3 - Caledonian Lower Cambrian clastic sediments. Distinct angular unconformity occus at the boundary between each of the structural units (figs 2 and 3). The investigated clastic sediments of Lower Cambrian (Buta, 1994; Bute & Jachowicz, 1995) and Lower Devonian (Tarnowska, 1989) consist of intercalated quartz sandstones, and mudstones with subordinate siltstones (Głedysz, 1984) (fig. 3). Structural investigations were also applied to dolomites which crop out in the Stare Gliny quarry (figs 2, 7h). Numerous generations of both sedimentary and tectonic structures have been distinguished in the investigated rocks (figs 4, 5 and 6). They include joint sets (kathetal joints and diagonal joints with features typical of shear joints), strike-slip mesofaults, and normal-slip faults, usually with tectonic breccia (figs 4-7). Fifteen episodes which constitute a geometrical-chronological sequence of different geological events, have been recognized. Based on them 8 stages of structural development of Lower Cambrian and Lower Devonian clastic sediments have been determined. Stage 1 includes sedimentation and diagenesis of Lower Cambrian rocks. Stage 2 was related to minor folding of Lower Cambrian rocks, most probably after early or after Middle Cambrian. Stage 3 involved denudation of Lower Cambrian rocks during late Cambrian, Ordovician and Sylurian. During stage 4 the sedimentation and diagenesis of Devonian rocks occurred. Stage 5 includes folding of both Lower Cambrian and Devonian formations, most probably between Early and Late Carboniferous or even after Namurian A (Oberc, 1993; Bukowy, 1994) under dextral transpresive regime (Żaba, 1994b, 1996). Stage 6 was related to the dextral shearing regime and occurred at the end of Visean (Żaba, 1994b, 1996). During stage 7 the subhorizontal and sinistral strike-slip brittle shear occurred under the sinistral transtensive regime (Żaba, 1994b) from late Carboniferous until early Triassic. The sinistral strike-slip brittle shear was also observed in granites of the edge zone of the Matopolska block (Żaba, 1994a). Stage 8 includes Alpine deformations whitch occurred after the earliest Triassic. Tectonic style of the investigated formations developed predominantly during the stage 5. At that stage the ChechłoGolczowice anticline formed.
Buła, Z.; Jachowicz-Zdanowska, M.; Żaba, J.
Principal characteristics of the Upper Silesian block and Małopolska block border zone (southern Poland) Journal Article
In: Geological Magazine, vol. 134, no. 5, pp. 669-677, 1997, ISSN: 00167568, (118).
@article{2-s2.0-0031430747,
title = {Principal characteristics of the Upper Silesian block and Małopolska block border zone (southern Poland)},
author = { Z. Buła and M. Jachowicz-Zdanowska and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0031430747&doi=10.1017%2fS0016756897007462&partnerID=40&md5=c0279e6acf3737823f706918fb11d5da},
doi = {10.1017/S0016756897007462},
issn = {00167568},
year = {1997},
date = {1997-01-01},
journal = {Geological Magazine},
volume = {134},
number = {5},
pages = {669-677},
publisher = {Cambridge University Press},
abstract = {The Upper Silesian and Małopolska blocks are situated near the southwestern boundary of the East European Platform within the Trans-European Suture Zone. The Lower Palaeozoic lithologies of the blocks reveal different stratigraphic and diastrophic development. In the Upper Silesian Block, unmetamorphosed and gently folded Lower Cambrian to Ordovician sedimentary rocks rest on a Cadomian basement. The Lower Cambrian is represented by an older (sub-Holmia) Borzȩta Formation and a younger (Holmia) Goczałkowice Formation. The thickness of the Cambrian lithologies increases from the southwest towards the lateral part of the block. In the Małopolska Block Palaeozoic and Precambrian lithologies are represented by regionally metamorphosed and intensely folded Lower Cambrian-Vendian clastic rocks which are unconformably overlain by Ordovician-Lower Silurian carbonates and Upper Silurian clastic rocks. The crystalline basement of the Małopolska Block has yet to be recognized. The Lower Palaeozoic sediments of both blocks are overlain by Devonian and Carboniferous rocks. The blocks are in direct contact along a narrow tectonic zone, a part of the largely concealed Hamburg-Kraków fault zone, in which tectonic evolution has taken place spasmodically with strike-slip movements predominating.},
note = {118},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Upper Silesian and Małopolska blocks are situated near the southwestern boundary of the East European Platform within the Trans-European Suture Zone. The Lower Palaeozoic lithologies of the blocks reveal different stratigraphic and diastrophic development. In the Upper Silesian Block, unmetamorphosed and gently folded Lower Cambrian to Ordovician sedimentary rocks rest on a Cadomian basement. The Lower Cambrian is represented by an older (sub-Holmia) Borzȩta Formation and a younger (Holmia) Goczałkowice Formation. The thickness of the Cambrian lithologies increases from the southwest towards the lateral part of the block. In the Małopolska Block Palaeozoic and Precambrian lithologies are represented by regionally metamorphosed and intensely folded Lower Cambrian-Vendian clastic rocks which are unconformably overlain by Ordovician-Lower Silurian carbonates and Upper Silurian clastic rocks. The crystalline basement of the Małopolska Block has yet to be recognized. The Lower Palaeozoic sediments of both blocks are overlain by Devonian and Carboniferous rocks. The blocks are in direct contact along a narrow tectonic zone, a part of the largely concealed Hamburg-Kraków fault zone, in which tectonic evolution has taken place spasmodically with strike-slip movements predominating.
Aleksandrowski, P.; Kryza, R.; Mazur, S.; Żaba, J.
Kinematic data on major Variscan strike-slip faults and shear zones in the Polish Sudetes, northeast Bohemian Massif Journal Article
In: Geological Magazine, vol. 134, no. 5, pp. 727-739, 1997, ISSN: 00167568, (130).
@article{2-s2.0-0031423502,
title = {Kinematic data on major Variscan strike-slip faults and shear zones in the Polish Sudetes, northeast Bohemian Massif},
author = { P. Aleksandrowski and R. Kryza and S. Mazur and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0031423502&doi=10.1017%2fS0016756897007590&partnerID=40&md5=1e17d60e91b64d8324459aea20e2f87f},
doi = {10.1017/S0016756897007590},
issn = {00167568},
year = {1997},
date = {1997-01-01},
journal = {Geological Magazine},
volume = {134},
number = {5},
pages = {727-739},
publisher = {Cambridge University Press},
abstract = {The still highly disputable terrane boundaries in the Sudetic segment of the Variscan belt mostly seem to follow major strike-slip faults and shear zones. Their kinematics, expected to place important constraints on the regional structural models, is discussed in some detail. The most conspicuous is the WNW-ESE Intra-Sudetic Fault Zone, separating several different structural units of the West Sudetes. It showed ductile dextral activity and, probably, displacement magnitude of the order of tens to hundreds kilometres, during late Devonian(?) to early Carboniferous times. In the late Carboniferous (to early Permian?), the sense of motion on the Intra-Sudetic Fault was reversed in a semi-brittle to brittle regime, with the left-lateral offset on the fault amounting to single kilometres. The north-south trending Niemcza and northeast-southwest Skrzynka shear zones are left-lateral, ductile features in the eastern part of the West Sudetes. Similarly oriented (northeast-southwest to NNE-SSW) regional size shear zones of as yet undetermined kinematics were discovered in boreholes under Cenozoic cover in the eastern part of the Sudetic foreland (the Niedźwiedź and Nysa-Brzeg shear zones). One of these is expected to represent the northern continuation of the major Stare Mesto Shear Zone in the Czech Republic, separating the geologically different units of the West and East Sudetes. The Rudawy Janowickie Metamorphic Unit, assumed in some reconstructions to comprise a mostly strike-slip terrane boundary, is characterized by ductile fabric developed in a thrusting regime, modified by a superimposed normal-slip extensional deformation. Thrusting-related deformational fabric was locally reoriented prior to the extensional event and shows present-day strike-slip kinematics in one of the sub-units. The Sudetic Boundary Fault, although prominent in the recent structure and topography of the region, was not active as a Variscan strike-slip fault zone. The reported data emphasize the importance of syn-orogenic strike-slip tectonics in the Sudetes. The recognized shear sense is compatible with a strike-slip model of the northeast margin of the Bohemian Massif, in which the Kaczawa and Góry Sowie Units underwent late Devonian-early Carboniferous southeastward long-distance displacement along the Intra-Sudetic Fault Zone from their hypothetical original position within the Northern Phyllite Zone and the Mid-German Crystalline High of the German Variscides, respectively, and were juxtaposed with units of different provenance southwest of the fault. The Intra-Sudetic Fault Zone, together with the Elbe Fault Zone further south, were subsequently cut in the east and their eastern segments were displaced and removed by the younger, early to late Carboniferous, NNE-SSW trending, transpressional Moldanubian-Stare Mesto Shear Zone.},
note = {130},
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pubstate = {published},
tppubtype = {article}
}
The still highly disputable terrane boundaries in the Sudetic segment of the Variscan belt mostly seem to follow major strike-slip faults and shear zones. Their kinematics, expected to place important constraints on the regional structural models, is discussed in some detail. The most conspicuous is the WNW-ESE Intra-Sudetic Fault Zone, separating several different structural units of the West Sudetes. It showed ductile dextral activity and, probably, displacement magnitude of the order of tens to hundreds kilometres, during late Devonian(?) to early Carboniferous times. In the late Carboniferous (to early Permian?), the sense of motion on the Intra-Sudetic Fault was reversed in a semi-brittle to brittle regime, with the left-lateral offset on the fault amounting to single kilometres. The north-south trending Niemcza and northeast-southwest Skrzynka shear zones are left-lateral, ductile features in the eastern part of the West Sudetes. Similarly oriented (northeast-southwest to NNE-SSW) regional size shear zones of as yet undetermined kinematics were discovered in boreholes under Cenozoic cover in the eastern part of the Sudetic foreland (the Niedźwiedź and Nysa-Brzeg shear zones). One of these is expected to represent the northern continuation of the major Stare Mesto Shear Zone in the Czech Republic, separating the geologically different units of the West and East Sudetes. The Rudawy Janowickie Metamorphic Unit, assumed in some reconstructions to comprise a mostly strike-slip terrane boundary, is characterized by ductile fabric developed in a thrusting regime, modified by a superimposed normal-slip extensional deformation. Thrusting-related deformational fabric was locally reoriented prior to the extensional event and shows present-day strike-slip kinematics in one of the sub-units. The Sudetic Boundary Fault, although prominent in the recent structure and topography of the region, was not active as a Variscan strike-slip fault zone. The reported data emphasize the importance of syn-orogenic strike-slip tectonics in the Sudetes. The recognized shear sense is compatible with a strike-slip model of the northeast margin of the Bohemian Massif, in which the Kaczawa and Góry Sowie Units underwent late Devonian-early Carboniferous southeastward long-distance displacement along the Intra-Sudetic Fault Zone from their hypothetical original position within the Northern Phyllite Zone and the Mid-German Crystalline High of the German Variscides, respectively, and were juxtaposed with units of different provenance southwest of the fault. The Intra-Sudetic Fault Zone, together with the Elbe Fault Zone further south, were subsequently cut in the east and their eastern segments were displaced and removed by the younger, early to late Carboniferous, NNE-SSW trending, transpressional Moldanubian-Stare Mesto Shear Zone.
1996
Żaba, J.
In: Przeglad Geologiczny, vol. 44, no. 2, pp. 173-180, 1996, ISSN: 00332151, (35).
@article{2-s2.0-0029750568,
title = {Late Carboniferous strike slip activity at the boundary zone of Upper Silesia and Małopolska Blocks [Późnokarbońska aktywność przesuwcza strefy granicznej bloków górnośla̧skiego i małopolskiego]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0029750568&partnerID=40&md5=2a68f408af6f491a1decdc0cff29e5e0},
issn = {00332151},
year = {1996},
date = {1996-01-01},
journal = {Przeglad Geologiczny},
volume = {44},
number = {2},
pages = {173-180},
abstract = {The edge (boundary) zone of the Małopolska Block (MB) and of the Upper Silesia Block (USB) is cut by two major, transcontinental fault zones: the Hamburg-Kraków and the Szczecin-Kraków-Prešov lineaments (Fig. 1). A longlasting tectonic activity of both these fault zones had an important impact on polyphase structural evolution of the edge zone area. Of particular intensity was their Late Carboniferous strike-slip motions, closely related to granitoid intrusions as well as to the accompanying ore mineralisations. The Late Carboniferous deformation comprised three stages during which a progressive rotation of horizontal compression axis took place. During the pre-intrusive stage, dated as posterior to Namurian A, under dextral transpressive regime conditions (NNE-SSW directed compression) the NE margin of the Upper Silesia Block was uplifted and overthrust along a high-angle reverse faults upon the edge of the Małopolska Block (Fig. 2). This produced fold and thrust structures (Figs 3 and 4) as well as Riedel shears and normal faults (Fig. 2) in the Palaeozoic strata. During the syn-intrusive stage, postdating the Westphalian B, in conditions of dextral transtension (NNW-SSE directed compression) granitoid bodies were emplaced in active, extensional shear zones (Figs 5-7), into voids produced in - beetwen en - echelon trains of penetrative P shears. The plutons intruded as well into pull-apart zones. These processes were accompanied by formation of R' and X shears. During the post-intrusive stage, which occurred at the turn of Westphalian and Stephanian and, most probably, also in the early Stephanian, under conditions of dextral simple shearing regime followed by dextral transpression (with horizontal compression axis direction oriented at first submeridianally, next replaced by NNE-SSW direction), the granitoids and their matle rocks were deformed (Figs 8-11 ). At that time several tectonic events produced folds, reverse faults and thrusts, parallel to analogous structures that had formed earlier during the pre-intrusive stage. A significant proportion of then generated faults were reactivated and rejuvenated older discontinuities. A saturated fault network developed at that stage. The main part was played at that time by the Szczecin-Kraków-Prešov fault zone. The displacements on the Hamburg-Kraków fault zone in the vicinities of Lubliniec were of the transpressive type, with initially sinistral strike-slip sense (at the pre-intrusive stage), being then replaced by dextral (at syn-intrusive stage) and, eventually, again by sinistral sense of motion (at the post-intrusive stage). At the syn-intrusive stage, at the same time when along the NE boundary of the Upper Silesia Block grainitoid plutons intruded under extensional regime, the western edge of this block was overriden, under compressional regime, by Early Carboniferous sediments of the Moravo-Silesian zone. The recently suggested Early Carboniferous large-scale strike-slip faulting in the Sudetes (Aleksandrowski 1990, 1994) along crustal discontinuities of the same direction (NW-SE to WNW-ESE) as those in the area under discussion, seems, therefore, to have migrated northwards in the Late Carboniferous and concentrated on the Odra fault zone and its continuation into the boundary faults between the Malopolska and Upper Silesia Blocks.},
note = {35},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The edge (boundary) zone of the Małopolska Block (MB) and of the Upper Silesia Block (USB) is cut by two major, transcontinental fault zones: the Hamburg-Kraków and the Szczecin-Kraków-Prešov lineaments (Fig. 1). A longlasting tectonic activity of both these fault zones had an important impact on polyphase structural evolution of the edge zone area. Of particular intensity was their Late Carboniferous strike-slip motions, closely related to granitoid intrusions as well as to the accompanying ore mineralisations. The Late Carboniferous deformation comprised three stages during which a progressive rotation of horizontal compression axis took place. During the pre-intrusive stage, dated as posterior to Namurian A, under dextral transpressive regime conditions (NNE-SSW directed compression) the NE margin of the Upper Silesia Block was uplifted and overthrust along a high-angle reverse faults upon the edge of the Małopolska Block (Fig. 2). This produced fold and thrust structures (Figs 3 and 4) as well as Riedel shears and normal faults (Fig. 2) in the Palaeozoic strata. During the syn-intrusive stage, postdating the Westphalian B, in conditions of dextral transtension (NNW-SSE directed compression) granitoid bodies were emplaced in active, extensional shear zones (Figs 5-7), into voids produced in - beetwen en - echelon trains of penetrative P shears. The plutons intruded as well into pull-apart zones. These processes were accompanied by formation of R' and X shears. During the post-intrusive stage, which occurred at the turn of Westphalian and Stephanian and, most probably, also in the early Stephanian, under conditions of dextral simple shearing regime followed by dextral transpression (with horizontal compression axis direction oriented at first submeridianally, next replaced by NNE-SSW direction), the granitoids and their matle rocks were deformed (Figs 8-11 ). At that time several tectonic events produced folds, reverse faults and thrusts, parallel to analogous structures that had formed earlier during the pre-intrusive stage. A significant proportion of then generated faults were reactivated and rejuvenated older discontinuities. A saturated fault network developed at that stage. The main part was played at that time by the Szczecin-Kraków-Prešov fault zone. The displacements on the Hamburg-Kraków fault zone in the vicinities of Lubliniec were of the transpressive type, with initially sinistral strike-slip sense (at the pre-intrusive stage), being then replaced by dextral (at syn-intrusive stage) and, eventually, again by sinistral sense of motion (at the post-intrusive stage). At the syn-intrusive stage, at the same time when along the NE boundary of the Upper Silesia Block grainitoid plutons intruded under extensional regime, the western edge of this block was overriden, under compressional regime, by Early Carboniferous sediments of the Moravo-Silesian zone. The recently suggested Early Carboniferous large-scale strike-slip faulting in the Sudetes (Aleksandrowski 1990, 1994) along crustal discontinuities of the same direction (NW-SE to WNW-ESE) as those in the area under discussion, seems, therefore, to have migrated northwards in the Late Carboniferous and concentrated on the Odra fault zone and its continuation into the boundary faults between the Malopolska and Upper Silesia Blocks.
1995
Żaba, J.
In: Przeglad Geologiczny, vol. 43, no. 10, pp. 838-842, 1995, ISSN: 00332151, (29).
@article{2-s2.0-0029476418,
title = {Strike-slip faults of the boundary zone of Upper Silesia and Malopolska blocks, southern Poland [Uskoki przesuwcze strefy krawedziowej blokow gornoslaskiego i malopolskiego]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0029476418&partnerID=40&md5=44492fd1564989dd92c7449f735b7bc6},
issn = {00332151},
year = {1995},
date = {1995-01-01},
journal = {Przeglad Geologiczny},
volume = {43},
number = {10},
pages = {838-842},
abstract = {The boundary zone between two base blocks of regional size, Malopolska (MB) and Upper Silesia (USB) is dissected by two major, transcontinental fault zones: the Hamburg-Krakow and the Czczecin-Krakow-Presov lineaments. The segment of the Hamburg-Krakow fault zone extending from Krakow to Lubliniec (Krakow-Lubliniec fault zone) separates the Upper Silesia block from the Malopolska block. The fault, most probably of Early Paleozoic or even Late Proterozoic foundations, showed particularly intense tectonic activity at the end of Silurian and during the Late Carboniferous. The Szczecin-Krakow-Presov fault zone transects the marginal area of the basement of the Upper Silesia block. It can be traced on gravimetric maps and topographic surface maps showing condensed topographic contours. The strike-slip fault zones played a long-lasting and important metallogenic role in the region. A direct spatial relationship to those major faults in shown, as well, by granitoid plutonism. At the end of the Variscan cycle, due to polyphase evolution of the Late Carboniferous, dextral, brittle strike-slip zone the regional fault network because so multidirectional and complex that during the younger deformation events was only able to reactivated along various older anisotropy directions. It was thus characterized by typical features of a saturated fault network. -from English summary},
note = {29},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The boundary zone between two base blocks of regional size, Malopolska (MB) and Upper Silesia (USB) is dissected by two major, transcontinental fault zones: the Hamburg-Krakow and the Czczecin-Krakow-Presov lineaments. The segment of the Hamburg-Krakow fault zone extending from Krakow to Lubliniec (Krakow-Lubliniec fault zone) separates the Upper Silesia block from the Malopolska block. The fault, most probably of Early Paleozoic or even Late Proterozoic foundations, showed particularly intense tectonic activity at the end of Silurian and during the Late Carboniferous. The Szczecin-Krakow-Presov fault zone transects the marginal area of the basement of the Upper Silesia block. It can be traced on gravimetric maps and topographic surface maps showing condensed topographic contours. The strike-slip fault zones played a long-lasting and important metallogenic role in the region. A direct spatial relationship to those major faults in shown, as well, by granitoid plutonism. At the end of the Variscan cycle, due to polyphase evolution of the Late Carboniferous, dextral, brittle strike-slip zone the regional fault network because so multidirectional and complex that during the younger deformation events was only able to reactivated along various older anisotropy directions. It was thus characterized by typical features of a saturated fault network. -from English summary
1994
Żaba, J.
In: Przeglad Geologiczny, vol. 8, pp. 638-642, 1994, ISSN: 00332151, (1).
@article{2-s2.0-0028574021,
title = {Premetamorphic stylolites in the Lower Paleozoic carbonate deposits of the Zawiercie, SW Poland [Przedmetamorficzne stylolity w dolnopaleozoicznych utworach weglanowych rejonu Zawiercia (NE obrzezenie GZW)]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0028574021&partnerID=40&md5=19de10097344dd7eb3651514f177b7b7},
issn = {00332151},
year = {1994},
date = {1994-01-01},
journal = {Przeglad Geologiczny},
volume = {8},
pages = {638-642},
abstract = {Two generations of the pre-metamorphic stylolites have been observed in limestones and marbles of the Ordovician-Silurian carbonate sequence. Older stylolites formed before folding or at the earliest stages of folding. Younger stylolites formed after folding of carbonates due to vertical stress caused by uplift of fragments of the crystalline basement of the Krakow-Myszkow fault zone. Orientation of the younger stylolites suggest that the NE part of the Krakow-Myszkow fault zone was uplifted. The formation of stylolites brought about shortening of the Lower Palaeozoic carbonate sequence by 0.7%. Both generations of stylolites were affected by the contact metamorphism. -English summary},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Two generations of the pre-metamorphic stylolites have been observed in limestones and marbles of the Ordovician-Silurian carbonate sequence. Older stylolites formed before folding or at the earliest stages of folding. Younger stylolites formed after folding of carbonates due to vertical stress caused by uplift of fragments of the crystalline basement of the Krakow-Myszkow fault zone. Orientation of the younger stylolites suggest that the NE part of the Krakow-Myszkow fault zone was uplifted. The formation of stylolites brought about shortening of the Lower Palaeozoic carbonate sequence by 0.7%. Both generations of stylolites were affected by the contact metamorphism. -English summary
Żaba, J.
In: Przeglad Geologiczny, vol. 8, pp. 643-648, 1994, ISSN: 00332151, (24).
@article{2-s2.0-0028563271,
title = {Mesoscopic flower structures in the Lower Paleozoic deposits of the NE border of the Upper Silesia Coal Basin - a result of the transpressional shearing in the Krakow-Myszkow (Hamburg-Krakow) dislocation zone, SW Poland [Mezoskopowe struktury kwiatowe w dolnopaleozoicznych utworach NE obrzezenia GZW - rezultat transpresyjnego scinania w strefie dyslokacyjnej Krakow-Myszkow (Hamburg-Krakow)]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0028563271&partnerID=40&md5=d1e4376e2e9d57e586ff27b7a03df4ec},
issn = {00332151},
year = {1994},
date = {1994-01-01},
journal = {Przeglad Geologiczny},
volume = {8},
pages = {643-648},
abstract = {Meso-scale positive flower structures have been observed in cores from unmetamorphosed to slighly metamorphosed Silurian flysch sequence in two boreholes located in the NE margin of the Upper Silesian Coal Basin in the vicinities of Myszkow (Z-63) and Zawiercie (RK-6). The boreholes were drilled within the major Hamburg-Krakow fault zone. The flower structures developed in rocks subjected to sinistral shear documented by low angle Riedel and P shears, strike-slip duplexes combined with reverse-slip movements on steep mesofaults. The formation of flower structures was preceded by folding and was succeeded by an extensional event. Determination of orientational parameters for one of the drill cores (RK-6) enabled assessment of prinicipal stress directions as well as the directions of shortening and extension. -from English summary},
note = {24},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Meso-scale positive flower structures have been observed in cores from unmetamorphosed to slighly metamorphosed Silurian flysch sequence in two boreholes located in the NE margin of the Upper Silesian Coal Basin in the vicinities of Myszkow (Z-63) and Zawiercie (RK-6). The boreholes were drilled within the major Hamburg-Krakow fault zone. The flower structures developed in rocks subjected to sinistral shear documented by low angle Riedel and P shears, strike-slip duplexes combined with reverse-slip movements on steep mesofaults. The formation of flower structures was preceded by folding and was succeeded by an extensional event. Determination of orientational parameters for one of the drill cores (RK-6) enabled assessment of prinicipal stress directions as well as the directions of shortening and extension. -from English summary
1988
Żaba, J.; Kuzak, R.
In: Kwartalnik Geologiczny, vol. 32, no. 3-4, pp. 635-654, 1988, ISSN: 00235873, (3).
@article{2-s2.0-0024182279,
title = {Structure of the middle part of the Szklarska Poreba slate range, Izera Mts [Budowa strukturalna srodkowej czesci pasma lupkowego Szklarskiej Poreby (Gory Izerskie)]},
author = { J. Żaba and R. Kuzak},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0024182279&partnerID=40&md5=0731d13eb8b872c8f5e1ae1277a82c2f},
issn = {00235873},
year = {1988},
date = {1988-01-01},
journal = {Kwartalnik Geologiczny},
volume = {32},
number = {3-4},
pages = {635-654},
abstract = {Four stages of tectonic deformation D1-D4 were distinguished, leading to development of mesofolds and corresponding planar structures. Morphology and spatial orientation of individual generations of mesostructures prove gradual development of deformations in varying field of forces and increasing competence of deformed rocks. Amidst sedimentary structures there are only planes of primary stratification S0 that seem to have forced directions of further tectonic deformations. Outside bend zones of folds these planes usually agree with penetrative foliation S1. In the studied area two dislocations of regional significance were noted. The fault of Czerwony Potok (CzP) is of rotation type, whilst the fault of Wysoki Kamien (WK) is probably of throw type. The type and timing of these deformations is discussed. -from English summary},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Four stages of tectonic deformation D1-D4 were distinguished, leading to development of mesofolds and corresponding planar structures. Morphology and spatial orientation of individual generations of mesostructures prove gradual development of deformations in varying field of forces and increasing competence of deformed rocks. Amidst sedimentary structures there are only planes of primary stratification S0 that seem to have forced directions of further tectonic deformations. Outside bend zones of folds these planes usually agree with penetrative foliation S1. In the studied area two dislocations of regional significance were noted. The fault of Czerwony Potok (CzP) is of rotation type, whilst the fault of Wysoki Kamien (WK) is probably of throw type. The type and timing of these deformations is discussed. -from English summary
1984
Żaba, J.
In: Geologia Sudetica, vol. 19, no. 2, pp. 89-192, 1984, ISSN: 0072100X, (11).
@article{2-s2.0-0021534801,
title = {Polish with English summary & abstract [(Genesis and metamorphic evolution of gneisses and granitoids of the Izerski Stog massif (Western Sudetes).)]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021534801&partnerID=40&md5=5bab827a1dc3767fa872a45d5fb18072},
issn = {0072100X},
year = {1984},
date = {1984-01-01},
journal = {Geologia Sudetica},
volume = {19},
number = {2},
pages = {89-192},
abstract = {Geological mapping, petrographic and petrochemical studies, mineral investigation and mesostructural analysis of the little-known massif of Izerski Stog have been carried out to explain the genesis and evolution of the rocks, particularly the gneisses and granites. The evolution of these rocks has been divided into nine stages: 1) geosynclinal; 2) Barrow-type regional metamorphism; 3) recrystallization; 4) retrogressive metamorphism; 5) microclinization and pegmatization; 6) regional metasomatism; 7) faint deformation; 8) local metasomatism and 9) contact metamorphism.-R.E.S.},
note = {11},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Geological mapping, petrographic and petrochemical studies, mineral investigation and mesostructural analysis of the little-known massif of Izerski Stog have been carried out to explain the genesis and evolution of the rocks, particularly the gneisses and granites. The evolution of these rocks has been divided into nine stages: 1) geosynclinal; 2) Barrow-type regional metamorphism; 3) recrystallization; 4) retrogressive metamorphism; 5) microclinization and pegmatization; 6) regional metasomatism; 7) faint deformation; 8) local metasomatism and 9) contact metamorphism.-R.E.S.
Żaba, J.
Some remarks on pre-Variscan contact metamorphism of rocks of the Izera block (western Sudetes). Journal Article
In: Bulletin of the Polish Academy of Sciences: Earth Sciences, vol. 32, no. 1-4, pp. 73-80, 1984, (3).
@article{2-s2.0-0021369992,
title = {Some remarks on pre-Variscan contact metamorphism of rocks of the Izera block (western Sudetes).},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0021369992&partnerID=40&md5=4098c8edcb02c16f921d5acf1930f905},
year = {1984},
date = {1984-01-01},
journal = {Bulletin of the Polish Academy of Sciences: Earth Sciences},
volume = {32},
number = {1-4},
pages = {73-80},
abstract = {The Polish pre-Variscan contact metamorphism caused by intrusions of palingenetic magma in mantle rocks approx 500-450 m.y. ago probably occurred in the K-feldspar-cordierite hornfels facies at 635o-655oC (locally up to 695oC) with PH2O approx 2.5 kbar at a depth of approx 9-10 km.-R.A.H.},
note = {3},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The Polish pre-Variscan contact metamorphism caused by intrusions of palingenetic magma in mantle rocks approx 500-450 m.y. ago probably occurred in the K-feldspar-cordierite hornfels facies at 635o-655oC (locally up to 695oC) with PH2O approx 2.5 kbar at a depth of approx 9-10 km.-R.A.H.
1983
Kozlowski, K.; Żaba, J.
Clinopyroxenes in skarn from the vicinity of Glucholazy (Eastern Sudetes). Journal Article
In: Bulletin of the Polish Academy of Sciences, Earth Sciences, vol. 31, no. 1-4, pp. 79-87, 1983, ISSN: 02397277.
@article{2-s2.0-0020859951,
title = {Clinopyroxenes in skarn from the vicinity of Glucholazy (Eastern Sudetes).},
author = { K. Kozlowski and J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0020859951&partnerID=40&md5=b1654e5e6ddba0a444b73fd90d5861fa},
issn = {02397277},
year = {1983},
date = {1983-01-01},
journal = {Bulletin of the Polish Academy of Sciences, Earth Sciences},
volume = {31},
number = {1-4},
pages = {79-87},
abstract = {Clinopyroxene crystals from this skarn have been analysed and found to contain diopside 73.70%, hedenbergite 22.33%, tschermakite 2.98% and acmite 0.99%. The optical properties are alpha 1.680, beta 1.685, gamma 1.704, gamma :c 40o. The diffractogram of this mineral indicates a pyroxene close to diopside with reflections shifted towards higher d-values. Fibrous amphiboles in the skarn belong to the tremolite-actinolite series and were formed as a result of secondary alterations of clinopyroxenes.-R.E.S.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
Clinopyroxene crystals from this skarn have been analysed and found to contain diopside 73.70%, hedenbergite 22.33%, tschermakite 2.98% and acmite 0.99%. The optical properties are alpha 1.680, beta 1.685, gamma 1.704, gamma :c 40o. The diffractogram of this mineral indicates a pyroxene close to diopside with reflections shifted towards higher d-values. Fibrous amphiboles in the skarn belong to the tremolite-actinolite series and were formed as a result of secondary alterations of clinopyroxenes.-R.E.S.
1982
Żaba, J.
Polish with English summary [(Proposed classification and nomenclature of the gneisses and granites of the Izera block (western Sudetes.)] Journal Article
In: Geologia Sudetica, vol. 17, no. 1-2, pp. 141-154, 1982, ISSN: 0072100X, (6).
@article{2-s2.0-0020387711,
title = {Polish with English summary [(Proposed classification and nomenclature of the gneisses and granites of the Izera block (western Sudetes.)]},
author = { J. Żaba},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0020387711&partnerID=40&md5=80851e36e622844e6edb89bb1775a405},
issn = {0072100X},
year = {1982},
date = {1982-01-01},
journal = {Geologia Sudetica},
volume = {17},
number = {1-2},
pages = {141-154},
abstract = {This classification of the gneisses and granites of this part of the Czech-Polish Sudetes Mts is based on the rock structures and colour index, but also includes grain size and size ratios between grains of individual rock-forming minerals. Rocks with directional structures are sub-divided into laminated, flaser-type and granite gneisses.-R.A.H.},
note = {6},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
This classification of the gneisses and granites of this part of the Czech-Polish Sudetes Mts is based on the rock structures and colour index, but also includes grain size and size ratios between grains of individual rock-forming minerals. Rocks with directional structures are sub-divided into laminated, flaser-type and granite gneisses.-R.A.H.