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  • The structure of the crust and the crust-mantle boundary in the Vogtland/West Bohemian region have been a target of several seismic measurements for the last 25 years, beginning with the steep-angle reflection seismic studies (DEKORP-4/KTB, MVE-90, 9HR), the refraction and wide-angle experiments (GRANU’95, CELEBRATION 2000, SUDETES 2003), and followed by passive seismic studies (receiver functions, teleseismic tomography). The steep-angle reflection studies imaged a highly reflective lower crust (4 to 6 km thick) with the Moho interpreted in a depth between 30 and 32 km and a thinner crust beneath the Eger Rift. The refraction and wide-angle reflection seismic studies (CELEBRATION 2000) revealed strong wide-angle reflections in a depth of 26–28 km interpreted as the top of the lower crust.
  • The structure of the crust and the crust-mantle boundary in the Vogtland/West Bohemian region have been a target of several seismic measurements for the last 25 years, beginning with the steep-angle reflection seismic studies (DEKORP-4/KTB, MVE-90, 9HR), the refraction and wide-angle experiments (GRANU’95, CELEBRATION 2000, SUDETES 2003), and followed by passive seismic studies (receiver functions, teleseismic tomography). The steep-angle reflection studies imaged a highly reflective lower crust (4 to 6 km thick) with the Moho interpreted in a depth between 30 and 32 km and a thinner crust beneath the Eger Rift. The refraction and wide-angle reflection seismic studies (CELEBRATION 2000) revealed strong wide-angle reflections in a depth of 26–28 km interpreted as the top of the lower crust. (en)
Title
  • The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods
  • The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods (en)
skos:prefLabel
  • The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods
  • The crust-mantle transition and the Moho beneath the Vogtland/West Bohemian region in the light of different seismic methods (en)
skos:notation
  • RIV/67985530:_____/09:00330249!RIV10-AV0-67985530
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA300120801), Z(AV0Z30120515)
http://linked.open...iv/cisloPeriodika
  • 3
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
  • 308588
http://linked.open...ai/riv/idVysledku
  • RIV/67985530:_____/09:00330249
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Bohemian Massif; Vogtland/West Bohemia; crustal structure; Moho; refraction and wide-angle reflection; receiver function; seismic methods; Eger Rift (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [CCC36E9B619A]
http://linked.open...i/riv/nazevZdroje
  • Studia geophysica et geodaetica
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
  • 53
http://linked.open...iv/tvurceVysledku
  • Hrubcová, Pavla
  • Geissler, W. H.
http://linked.open...ain/vavai/riv/wos
  • 000268584800001
http://linked.open...n/vavai/riv/zamer
issn
  • 0039-3169
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