About: Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia)     Goto   Sponge   NotDistinct   Permalink

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  • This paper focuses on the comparison of the magnetic susceptibility (MS) curves over a large distance and across the facies. The Ardennes section shows an alternation of near shore platform, ramp and mound environments where detrital inputs are very important. Time-equivalent facies in the area of the Moravian Karst correspond to high purity limestones of open-sea platform type where Amphipora beds dominated shallow reef interior. In spite of these differences, the Eifelian-Frasnian MS pattern successions of Belgium have a great similarity to Moravia. The atmospheric circulation of dust and its widespread distribution on the Devonian globe is an appropriate mechanism through which this continuity can be explained.
  • This paper focuses on the comparison of the magnetic susceptibility (MS) curves over a large distance and across the facies. The Ardennes section shows an alternation of near shore platform, ramp and mound environments where detrital inputs are very important. Time-equivalent facies in the area of the Moravian Karst correspond to high purity limestones of open-sea platform type where Amphipora beds dominated shallow reef interior. In spite of these differences, the Eifelian-Frasnian MS pattern successions of Belgium have a great similarity to Moravia. The atmospheric circulation of dust and its widespread distribution on the Devonian globe is an appropriate mechanism through which this continuity can be explained. (en)
Title
  • Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia)
  • Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia) (en)
skos:prefLabel
  • Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia)
  • Magnetic susceptibility correlation of km-thick Eifelian–Frasnian sections (Ardennes and Moravia) (en)
skos:notation
  • RIV/67985831:_____/10:00345505!RIV11-AV0-67985831
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA300130702), P(IAAX00130702), Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • 4
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
  • 269193
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/10:00345505
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Devonian limestone; magnetic susceptibility; Moravian Karst; Ardennes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • BE - Belgické království
http://linked.open...ontrolniKodProRIV
  • [ED17A3214957]
http://linked.open...i/riv/nazevZdroje
  • GEOLOGICA BELGICA
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
  • 13
http://linked.open...iv/tvurceVysledku
  • Geršl, M.
  • Hladil, Jindřich
  • Koptíková, Leona
  • Schnabl, Petr
  • Boulvain, F.
  • Mabille, C.
  • da Silva, A. C.
http://linked.open...ain/vavai/riv/wos
  • 000285908500003
http://linked.open...n/vavai/riv/zamer
issn
  • 1374-8505
number of pages
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