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Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation
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SYSNO ASEP 0365873 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation Author(s) Novotný, Miroslav (GFU-E) RID Source Title Surveys in Geophysics. - : Springer - ISSN 0169-3298
Roč. 33, č. 2 (2012), s. 243-273Number of pages 31 s. Publication form Print - P Language eng - English Country NL - Netherlands Keywords depth-recursive refraction tomography ; Bohemian Massif ; CEL09 profile Subject RIV DC - Siesmology, Volcanology, Earth Structure R&D Projects LA08036 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000305535100002 DOI 10.1007/s10712-011-9155-x Annotation In the accompanying paper (Part A), depth-recursive tomography was applied to the CEL09 refraction data. A deblurred P-wave velocity image was obtained down to a depth of 20 km. This paper (Part B) is devoted to the interpretation of the upper- and middle-crustal structures of the Bohemian Massif imaged in the CEL09 section. Because of inherent ambiguity of the refraction method in imaging low-velocity zones, other wellknown results based on other geophysical data sets are also used to independently verify the interpreted velocity features. Comparison with the density and velocity models previously obtained indicates that the presented P-wave velocity image has superior resolution revealing or verifying a number of geological features. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2013
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