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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 ASEP0330249
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleThe 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 TitleStudia geophysica et geodaetica. - : Geofyzikální ústav AV ČR, v. v. i. - ISSN 0039-3169
    Roč. 53, č. 3 (2009), s. 275-294
    Number of pages20 s.
    Languageeng - English
    CountryCZ - Czech Republic
    KeywordsBohemian Massif ; Vogtland/West Bohemia ; crustal structure ; Moho ; refraction and wide-angle reflection ; receiver function ; seismic methods ; Eger Rift
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    R&D ProjectsIAA300120801 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    UT WOS000268584800001
    DOI10.1007/s11200-009-0018-6
    AnnotationThe 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.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2010
Number of the records: 1  

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