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New geophysical and geological data on the Moldanubian plutonic complex and the Kaplice Fault, southern Bohemia
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SYSNO ASEP 0557454 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title New geophysical and geological data on the Moldanubian plutonic complex and the Kaplice Fault, southern Bohemia Author(s) Melnyk, A. (CZ)
Černý, Jan (GLU-S) RID, ORCID, SAI
Pospíšil, L. (CZ)
Adamovič, Jiří (GLU-S) RID, SAI, ORCIDSource Title International Journal of Earth Sciences. - : Springer - ISSN 1437-3254
Roč. 111, č. 4 (2022), s. 1315-1331Number of pages 17 s. Publication form Print - P Language eng - English Country DE - Germany Keywords Geophysics ; Gravity ; Granite ; Plutonic complex ; Moldanubicum ; Kaplice Fault OECD category Geology R&D Projects GJ19-02177Y GA ČR - Czech Science Foundation (CSF) Method of publishing Limited access Institutional support GLU-S - RVO:67985831 UT WOS 000773838800002 EID SCOPUS 85127253308 DOI 10.1007/s00531-022-02182-5 Annotation The paper presents a new structural model of the granitoid intrusions of the Moldanubian plutonic complex in southern Bohemiaeast of the town of Kaplice. Valuable archival gravity data were supplemented by magnetic survey and precise profile gravity measurements to better define the gravitational effect of the granitoid body and provide an accurate model solution. Our findings, based on geophysical analyses and modelling, bring new information on the shape and deep structure of the Moldanubian plutonic complex in southern Bohemia. These results are complemented by a tectonic investigation of the Freistadt granodiorite body and the Kaplice Fault. New information on the geometry of the Kaplice Fault plane acquired from Linsser indications is discussed in relation to its possible recent seismic activity. The usefulness of the Linsser indications method for active tectonic studies is demonstrated. This is the first regional study in this insufficiently known part of the Bohemian Massif, providing new information on the extent of granites and their relationship to one of the most significant faults in this area. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2023 Electronic address https://link.springer.com/article/10.1007/s00531-022-02182-5
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