About: Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation     Goto   Sponge   NotDistinct   Permalink

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Description
  • 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.
  • 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. (en)
Title
  • Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation
  • Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation (en)
skos:prefLabel
  • Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation
  • Depth-recursive tomography of the Bohemian Massif at the CEL09 transect—Part B: Interpretation (en)
skos:notation
  • RIV/67985530:_____/12:00365873!RIV13-AV0-67985530
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(LA08036), Z(AV0Z30120515)
http://linked.open...iv/cisloPeriodika
  • 2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 130143
http://linked.open...ai/riv/idVysledku
  • RIV/67985530:_____/12:00365873
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • depth-recursive refraction tomography; Bohemian Massif; CEL09 profile (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [8A9597C2D365]
http://linked.open...i/riv/nazevZdroje
  • Surveys in Geophysics
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 33
http://linked.open...iv/tvurceVysledku
  • Novotný, Miroslav
http://linked.open...ain/vavai/riv/wos
  • 000305535100002
http://linked.open...n/vavai/riv/zamer
issn
  • 0169-3298
number of pages
http://bibframe.org/vocab/doi
  • 10.1007/s10712-011-9155-x
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