About: Vinařická hora Hill Cenozoic Composite Volcano, Central Bohemia: Geochemical Contraints.     Goto   Sponge   Distinct   Permalink

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  • Olivine-poor nephelinite of Vinařická hora Hill substantially differs from both olivine nephelinite and olivine-free nephelinite of the Cenozoic volcanic province of the Bohemian Massif. Vinařická hora Hill represents a volcanic relict 31.0-25.5 Ma in age located in the Bohemian Cretaceous Basin in central Bohemian area. The very low Mg-value (46.6-49.7), low contents of compatible elements such as Cr(4.9-23.3), Ni(3-55), Co(39-43), Sc(17.0-18.6)(all data in Mu.g g1) and the lack of mantle-type xenoliths evidence differentiation of primary mantel magma. Anomalous enrichment in incompatible elements, particulary in SIGMA.REE (523-589), Zr(601-842), U(2.1-3.1), Th(11.6-13.0), Nb(176-188), Ta(10.5-11.2), is associated with magmatic differentiation manifested in crystallization of apatite, Ti-magnetite + hauyne(?). Olivine-poor nephelinite could be derived from carbonated naphelinite magma with high COH2O + CO2 volatile fraction resulting in high viscosity and consequent stopping of magma associated with
  • Olivine-poor nephelinite of Vinařická hora Hill substantially differs from both olivine nephelinite and olivine-free nephelinite of the Cenozoic volcanic province of the Bohemian Massif. Vinařická hora Hill represents a volcanic relict 31.0-25.5 Ma in age located in the Bohemian Cretaceous Basin in central Bohemian area. The very low Mg-value (46.6-49.7), low contents of compatible elements such as Cr(4.9-23.3), Ni(3-55), Co(39-43), Sc(17.0-18.6)(all data in Mu.g g1) and the lack of mantle-type xenoliths evidence differentiation of primary mantel magma. Anomalous enrichment in incompatible elements, particulary in SIGMA.REE (523-589), Zr(601-842), U(2.1-3.1), Th(11.6-13.0), Nb(176-188), Ta(10.5-11.2), is associated with magmatic differentiation manifested in crystallization of apatite, Ti-magnetite + hauyne(?). Olivine-poor nephelinite could be derived from carbonated naphelinite magma with high COH2O + CO2 volatile fraction resulting in high viscosity and consequent stopping of magma associated with (en)
Title
  • Vinařická hora Hill Cenozoic Composite Volcano, Central Bohemia: Geochemical Contraints.
  • Vinařická hora Hill Cenozoic Composite Volcano, Central Bohemia: Geochemical Contraints. (en)
skos:prefLabel
  • Vinařická hora Hill Cenozoic Composite Volcano, Central Bohemia: Geochemical Contraints.
  • Vinařická hora Hill Cenozoic Composite Volcano, Central Bohemia: Geochemical Contraints. (en)
skos:notation
  • RIV/61389005:_____/03:49033077!RIV/2004/AV0/A49004/N
http://linked.open.../vavai/riv/strany
  • 126
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA3048201), Z(AV0Z1048901), Z(AV0Z3013912)
http://linked.open...iv/cisloPeriodika
  • N/A
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http://linked.open...dnocenehoVysledku
  • 633032
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  • RIV/61389005:_____/03:49033077
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  • Bohemian massif; Vinařická hora Hill; geochemistry (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
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  • [E7468958D946]
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  • GeoLines
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http://linked.open...vavai/riv/projekt
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http://linked.open...v/svazekPeriodika
  • 15
http://linked.open...iv/tvurceVysledku
  • Kučera, Jan
  • Řanda, Zdeněk
  • Frána, Jaroslav
  • Balogh, K.
  • Ulrych, Jaromír
  • Novák, Jiří Karel
http://linked.open...n/vavai/riv/zamer
issn
  • 1210-9606
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