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Links between the structure of the mantle lithosphere and morphology of the Cheb Basin (Eger Rift, central Europe)
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SYSNO ASEP 0342694 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Links between the structure of the mantle lithosphere and morphology of the Cheb Basin (Eger Rift, central Europe) Author(s) Babuška, Vladislav (GFU-E) ORCID, RID, SAI
Plomerová, Jaroslava (GFU-E) ORCID, RID, SAI
Vecsey, Luděk (GFU-E) ORCID, RID, SAISource Title International Journal of Earth Sciences. - : Springer - ISSN 1437-3254
Roč. 99, č. 7 (2010), s. 1535-1544Number of pages 10 s. Language eng - English Country DE - Germany Keywords Western Bohemian Massif ; Eger (Ohře) Rift ; Cheb Basin ; surface morphology ; mantle lithosphere Subject RIV DC - Siesmology, Volcanology, Earth Structure R&D Projects GA205/07/1088 GA ČR - Czech Science Foundation (CSF) IAA300120709 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000282701900005 DOI 10.1007/s00531-010-0531-4 Annotation The Cheb Basin (CHB), located in the western part of the Eger Rift (ER) and the western Bohemian Massif, is characterized by earthquake swarms, neotectonic crust movements and emanations of CO2 dominated gases of mantle origin. Deep structure of the region can be characterized as junction of three domains of mantle lithosphere with different olivine fabrics revealed by consistent orientations of seismic anisotropy. The domains represent mantle components of the major tectonic units (micro-plates): Saxothuringian (ST), Teplá-Barrandian (TB) and Moldanubian (MD), which were assembled during the Variscan orogeny. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2011
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