About: Late Miocene volcanic activity in the České středohoří Mountains (Ohře/Eger Graben, Northern Bohemia)     Goto   Sponge   NotDistinct   Permalink

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  • First occurrences of superficial bodies of Late Miocene volcanic activity were found in the w. part of the České středohoří Volcanic Complex. Their K-Ar ages (9.59, 9.61 and 11.36 Ma) correspond to the age of alkaline basaltic rocks of the youngest known Intrusive System of this area. These bodies are represented by superficial products: two scoria cones with remnants of lava flows and one exclusive lava flow produced from a lava cone. Their primitive (basanitic) chemical composition, Sr (0.70347 – 0.70361) and Nd (0.51279 – 0,51284) isotope ratios are similar to the products of the first and third volcanic formation of the CSVC. The proved existence of superficial products, together with clear superposition relations to sedimentary formations and the chemical character of the youngest magmas support the stratigraphic scheme of volcanic activity in the České středohoří Mts. Eruptive style of the youngest formation volcanoes was purely magmatic (Strombolian) with no phreatic influence.
  • First occurrences of superficial bodies of Late Miocene volcanic activity were found in the w. part of the České středohoří Volcanic Complex. Their K-Ar ages (9.59, 9.61 and 11.36 Ma) correspond to the age of alkaline basaltic rocks of the youngest known Intrusive System of this area. These bodies are represented by superficial products: two scoria cones with remnants of lava flows and one exclusive lava flow produced from a lava cone. Their primitive (basanitic) chemical composition, Sr (0.70347 – 0.70361) and Nd (0.51279 – 0,51284) isotope ratios are similar to the products of the first and third volcanic formation of the CSVC. The proved existence of superficial products, together with clear superposition relations to sedimentary formations and the chemical character of the youngest magmas support the stratigraphic scheme of volcanic activity in the České středohoří Mts. Eruptive style of the youngest formation volcanoes was purely magmatic (Strombolian) with no phreatic influence. (en)
Title
  • Late Miocene volcanic activity in the České středohoří Mountains (Ohře/Eger Graben, Northern Bohemia)
  • Late Miocene volcanic activity in the České středohoří Mountains (Ohře/Eger Graben, Northern Bohemia) (en)
skos:prefLabel
  • Late Miocene volcanic activity in the České středohoří Mountains (Ohře/Eger Graben, Northern Bohemia)
  • Late Miocene volcanic activity in the České středohoří Mountains (Ohře/Eger Graben, Northern Bohemia) (en)
skos:notation
  • RIV/00025798:_____/09:00000163!RIV10-MZP-00025798
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA300130612), Z(AV0Z30130516), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 6
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
  • 323289
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/09:00000163
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • volcanostratigraphy, geochemistry, K-Ar dating, České středohoří , Upper Miocene, Štrbice Formation, cinder cone, basanite (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • SK - Slovenská republika
http://linked.open...ontrolniKodProRIV
  • [F9B5E9D782A1]
http://linked.open...i/riv/nazevZdroje
  • Geologica Carpathica
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
  • 60
http://linked.open...iv/tvurceVysledku
  • Erban, Vojtěch
  • Rapprich, Vladislav
  • Radoň, Miroslav
  • Pécskay, Zoltán
  • Cajz, Vladimír
http://linked.open...ain/vavai/riv/wos
  • 000274039600007
http://linked.open...n/vavai/riv/zamer
issn
  • 1335-0552
number of pages
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