The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods

0330249 - GFÚ 2010 RIV CZ eng J - Článek v odborném periodiku
Hrubcová, Pavla - Geissler, W.H.
The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods.
Studia geophysica et geodaetica. Roč. 53, č. 3 (2009), s. 275-294. ISSN 0039-3169. E-ISSN 1573-1626
Grant CEP: GA AV ČR IAA300120801
Výzkumný záměr: CEZ:AV0Z30120515
Klíčová slova: Bohemian Massif * Vogtland/West Bohemia * crustal structure * Moho * refraction and wide-angle reflection * receiver function * seismic methods * Eger Rift
Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
Impakt faktor: 1.000, rok: 2009

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.
Trvalý link: http://hdl.handle.net/11104/0176079