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

  1. 1.
    0365873 - GFÚ 2013 RIV NL eng J - Článek v odborném periodiku
    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
    Grant CEP: GA MŠMT LA08036
    Výzkumný záměr: CEZ:AV0Z30120515
    Klíčová slova: depth-recursive refraction tomography * Bohemian Massif * CEL09 profile
    Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
    Impakt faktor: 4.125, rok: 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.
    Trvalý link: http://hdl.handle.net/11104/0201016

     
     
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