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Lithosphere structure of the NE Bohemian Massif (Sudetes) — A teleseismic receiver function study
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SYSNO ASEP 0381573 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Lithosphere structure of the NE Bohemian Massif (Sudetes) — A teleseismic receiver function study Author(s) Geissler, W.H. (DE)
Kämpf, H. (DE)
Skácelová, Z. (CZ)
Plomerová, Jaroslava (GFU-E) ORCID, RID, SAI
Babuška, Vladislav (GFU-E) ORCID, RID, SAI
Kind, R. (DE)Source Title Tectonophysics. - : Elsevier - ISSN 0040-1951
564-565, Sep 5 (2012), s. 12-37Number of pages 26 s. Publication form Print - P Language eng - English Country NL - Netherlands Keywords lithospheric structure ; Moho discontinuity ; lithosphere-asthenosphere boundary ; Permo-Carboniferous volcanism ; Central Europe Subject RIV DC - Siesmology, Volcanology, Earth Structure R&D Projects GA205/07/1088 GA ČR - Czech Science Foundation (CSF) GAP210/12/2381 GA ČR - Czech Science Foundation (CSF) LM2010008 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000308681600002 DOI https://doi.org/10.1016/j.tecto.2012.05.005 Annotation In 2004 and 2005 a passive seismic experiment was carried out in the northern and northeastern part of the Bohemian Massif (Sudetes) to study the lithospheric structure. We present results from Ps and Sp receiver function analyses. With one exception, Moho depth at stations in the northwestern part of the study area varies between 28 and 32 km. Thicker crust up to 35 km was mapped toward the south (Moldanubian unit) and toward the east (Moravo–Silesian and Brunovistulian units) confirming results from previous active seismic measurements. There exists a relatively sharp step in Moho depth between units of the central Sudetes. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2013
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