Crustal structures beneath the Saxonian Granulite Massif, the České středohoří and the Doupovské hory Mts. based on the depth-recursive tomography

0348528 - GFÚ 2011 RIV CZ eng J - Journal Article
Novotný, Miroslav - Skácelová, Z. - Mlčoch, B.
Crustal structures beneath the Saxonian Granulite Massif, the České středohoří and the Doupovské hory Mts. based on the depth-recursive tomography.
Journal of Geosciences. Roč. 55, č. 3 (2010), s. 187-199. ISSN 1802-6222. E-ISSN 1803-1943
R&D Projects: GA AV ČR IAA300460602; GA MŽP SB/630/3/02
Grant - others:GA Mšk(CZ) 1M0554
Program: 1M
Institutional research plan: CEZ:AV0Z30120515
Keywords : depth-recursive refraction tomography * SUDETES 2003 seismic profiles S04 and S01 * Bohemian Massif * Saxonian Granulite Massif * Altenberg-Teplice Caldera * České středohoří and Doupovské hory volcanic complexes
Subject RIV: DC - Siesmology, Volcanology, Earth Structure
Impact factor: 1.026, year: 2010

The P-wave velocity distribution, obtained recently by the depth-recursive tomography along the S01 refraction profile of the SUDETES 2003 seismic experiment, correlated fairly well with other geophysical results known in the area of the KTB deep drilling site. The S01 velocity model also provided a reliable velocity image of the upper and middle-crustal structures along the Eger Graben. In the present paper we will use the results of the depth-recursive tomography applied to the crossing S04 profile to derive a 3-D picture of structures near the S04 and S01 intersection.
Permanent Link: http://hdl.handle.net/11104/0189047