Depth-recursive tomography along the Eger Rift using the S01 profile refraction data: tested at the KTB super drilling hole, structural interpretation supported by magnetic, gravity and petrophysical data

0330159 - GFÚ 2010 RIV NL eng J - Journal Article
Novotný, Miroslav - Skácelová, Z. - Mrlina, Jan - Mlčoch, B. - Růžek, Bohuslav
Depth-recursive tomography along the Eger Rift using the S01 profile refraction data: tested at the KTB super drilling hole, structural interpretation supported by magnetic, gravity and petrophysical data.
Surveys in Geophysics. Roč. 30, č. 6 (2009), s. 561-600. ISSN 0169-3298. E-ISSN 1573-0956
R&D Projects: GA AV ČR IAA300460602; GA MŽP SB/630/3/02
Institutional research plan: CEZ:AV0Z30120515
Keywords : depth-recursive refraction tomography * lateral resolution * German Continental Deep Drilling Project (KTB) * Zone Erbendorf-Vohenstrauss (ZEV) * low-velocity zones
Subject RIV: DC - Siesmology, Volcanology, Earth Structure
Impact factor: 3.179, year: 2009

The refraction data from the SUDETES 2003 experiment were used for highresolution tomography along the profile S01. The S01 profile crosses the zone Erbendorf- Vohenstrauss (ZEV) near the KTB site, then follows the SW–NE oriented Eger Rift in the middle part and continues toward the NE across the Elbe zone and the Sudetic structures as far as the Trans-European Suture Zone. To get the best resolution in the velocity image only the first arrivals of Pg waves with minimum picking errors were used.
Permanent Link: http://hdl.handle.net/11104/0176008