Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides)
The geological map of the Klenov Pluton (Moldanubian Batholith), and its 3D visualization, brings the new findings in the context of granite emplacement within late-Variscan settings. The Klenov Pluton has a peraluminous composition resulting from partial melting of metasedimentary sources and subse...
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Taylor & Francis Group
2024-12-01
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| Series: | Journal of Maps |
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| Online Access: | https://www.tandfonline.com/doi/10.1080/17445647.2024.2317144 |
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| author | Jaroslava Pertoldová Kryštof Verner David Buriánek Jan Valenta Barbora Dudíková Zuzana Skácelová Jan Jelének Jan Jelínek Kenneth Johnson Otmar Petyniak Petra Hejtmánková |
| author_facet | Jaroslava Pertoldová Kryštof Verner David Buriánek Jan Valenta Barbora Dudíková Zuzana Skácelová Jan Jelének Jan Jelínek Kenneth Johnson Otmar Petyniak Petra Hejtmánková |
| author_sort | Jaroslava Pertoldová |
| collection | DOAJ |
| description | The geological map of the Klenov Pluton (Moldanubian Batholith), and its 3D visualization, brings the new findings in the context of granite emplacement within late-Variscan settings. The Klenov Pluton has a peraluminous composition resulting from partial melting of metasedimentary sources and subsequent differentiation. The new ages 327.14 ± 0.21 Ma and 327.80 ± 0.37 Ma, reflect the narrow time-span of magma emplacement and cooling. The 327 Ma Klenov Pluton was emplaced syntectonically as a ‘sheet-like’ granite intrusion at depth ca. 10 kilometers during the later stages of the Pelhřimov Core Complex exhumation (at ca. 329 to 327 Ma) associated with ∼N–S oriented compression. Gravity modelling suggests that the Klenov Pluton has an asymmetric shape where its western flank is parallel to the ∼NW moderately dipping Pelhřimov Core Complex. The eastern margin of the Pluton is shallower and has been later modified by ∼SE-side-up normal faulting (Lodhéřov Fault Zone). |
| format | Article |
| id | doaj-art-56bd955eda494e76a24a501220ea1b84 |
| institution | Kabale University |
| issn | 1744-5647 |
| language | English |
| publishDate | 2024-12-01 |
| publisher | Taylor & Francis Group |
| record_format | Article |
| series | Journal of Maps |
| spelling | doaj-art-56bd955eda494e76a24a501220ea1b842025-01-06T14:32:05ZengTaylor & Francis GroupJournal of Maps1744-56472024-12-0120110.1080/17445647.2024.2317144Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides)Jaroslava Pertoldová0Kryštof Verner1David Buriánek2Jan Valenta3Barbora Dudíková4Zuzana Skácelová5Jan Jelének6Jan Jelínek7Kenneth Johnson8Otmar Petyniak9Petra Hejtmánková10Czech Geological Survey, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicFaculty of Science, Institute of Engineering Geology, Hydrogeology and Applied Geophysics, Charles University, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicDepartment of Natural Sciences, University of Houston-Downtown, Houston, TX, USACzech Geological Survey, Prague, Czech RepublicCzech Geological Survey, Prague, Czech RepublicThe geological map of the Klenov Pluton (Moldanubian Batholith), and its 3D visualization, brings the new findings in the context of granite emplacement within late-Variscan settings. The Klenov Pluton has a peraluminous composition resulting from partial melting of metasedimentary sources and subsequent differentiation. The new ages 327.14 ± 0.21 Ma and 327.80 ± 0.37 Ma, reflect the narrow time-span of magma emplacement and cooling. The 327 Ma Klenov Pluton was emplaced syntectonically as a ‘sheet-like’ granite intrusion at depth ca. 10 kilometers during the later stages of the Pelhřimov Core Complex exhumation (at ca. 329 to 327 Ma) associated with ∼N–S oriented compression. Gravity modelling suggests that the Klenov Pluton has an asymmetric shape where its western flank is parallel to the ∼NW moderately dipping Pelhřimov Core Complex. The eastern margin of the Pluton is shallower and has been later modified by ∼SE-side-up normal faulting (Lodhéřov Fault Zone).https://www.tandfonline.com/doi/10.1080/17445647.2024.2317144Bohemian MassifMoldanubian ZoneKlenov Plutongeological mapfabric patterngeophysical survey |
| spellingShingle | Jaroslava Pertoldová Kryštof Verner David Buriánek Jan Valenta Barbora Dudíková Zuzana Skácelová Jan Jelének Jan Jelínek Kenneth Johnson Otmar Petyniak Petra Hejtmánková Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides) Journal of Maps Bohemian Massif Moldanubian Zone Klenov Pluton geological map fabric pattern geophysical survey |
| title | Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides) |
| title_full | Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides) |
| title_fullStr | Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides) |
| title_full_unstemmed | Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides) |
| title_short | Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides) |
| title_sort | geology u pb dating and 3d visualisation of late orogenic klenov pluton pelhrimov core complex central european variscides |
| topic | Bohemian Massif Moldanubian Zone Klenov Pluton geological map fabric pattern geophysical survey |
| url | https://www.tandfonline.com/doi/10.1080/17445647.2024.2317144 |
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