Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation

0365873 - GFÚ 2013 RIV NL eng J - Journal Article
Novotný, Miroslav
Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation.
Surveys in Geophysics. Roč. 33, č. 2 (2012), s. 243-273. ISSN 0169-3298. E-ISSN 1573-0956
R&D Projects: GA MŠMT LA08036
Institutional research plan: CEZ:AV0Z30120515
Keywords : depth-recursive refraction tomography * Bohemian Massif * CEL09 profile
Subject RIV: DC - Siesmology, Volcanology, Earth Structure
Impact factor: 4.125, year: 2012

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.
Permanent Link: http://hdl.handle.net/11104/0201016