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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
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SYSNO ASEP 0330159 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title 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 Author(s) Novotný, Miroslav (GFU-E) RID
Skácelová, Z. (CZ)
Mrlina, Jan (GFU-E) ORCID, RID
Mlčoch, B. (CZ)
Růžek, Bohuslav (GFU-E) ORCID, RIDSource Title Surveys in Geophysics. - : Springer - ISSN 0169-3298
Roč. 30, č. 6 (2009), s. 561-600Number of pages 40 s. Language eng - English Country NL - Netherlands 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 R&D Projects IAA300460602 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) SB/630/3/02 GA MŽP - Ministry of Environment (MŽP) CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000271119200002 DOI 10.1007/s10712-009-9068-0 Annotation 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. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2010
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