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The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods
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SYSNO ASEP 0330249 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods Author(s) Hrubcová, Pavla (GFU-E) ORCID, RID
Geissler, W.H. (DE)Source Title Studia geophysica et geodaetica. - : Geofyzikální ústav AV ČR, v. v. i. - ISSN 0039-3169
Roč. 53, č. 3 (2009), s. 275-294Number of pages 20 s. Language eng - English Country CZ - Czech Republic Keywords Bohemian Massif ; Vogtland/West Bohemia ; crustal structure ; Moho ; refraction and wide-angle reflection ; receiver function ; seismic methods ; Eger Rift Subject RIV DC - Siesmology, Volcanology, Earth Structure R&D Projects IAA300120801 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000268584800001 DOI 10.1007/s11200-009-0018-6 Annotation The structure of the crust and the crust-mantle boundary in the Vogtland/West Bohemian region have been a target of several seismic measurements for the last 25 years, beginning with the steep-angle reflection seismic studies (DEKORP-4/KTB, MVE-90, 9HR), the refraction and wide-angle experiments (GRANU’95, CELEBRATION 2000, SUDETES 2003), and followed by passive seismic studies (receiver functions, teleseismic tomography). The steep-angle reflection studies imaged a highly reflective lower crust (4 to 6 km thick) with the Moho interpreted in a depth between 30 and 32 km and a thinner crust beneath the Eger Rift. The refraction and wide-angle reflection seismic studies (CELEBRATION 2000) revealed strong wide-angle reflections in a depth of 26–28 km interpreted as the top of the lower crust. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2010
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