About: Litho-stratigraphic effect on Variscan fluid flow within the Prague synform, Barrandian: Evidence based on C, O, Sr isotopes and fluid inclusions     Goto   Sponge   NotDistinct   Permalink

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  • The Palaeozoic sedimentary sequence of the Prague synform (Ordovician- Devonian) in the centre of the Bohemian massif underwent Variscan deformation and thermal overprint events. Variscan veins widespread throughout the sedimentary strata have precipitated from syntectonic aqueous and hydrocarbon-rich fluids. Homogenization temperatures of aqueous inclusions increased from 70 up to 226 degC in the Cambrian rocks underlying the Prague synform. Seawater, modified due to intensive water-rock interaction, was the main fluid component. Fluid flow was limited and restricted to the lithostratigraphic compartments forming a rock-buffered system. Stable isotopic modelling (C, O) and final interpretations of the confined hydrostratigraphic fluid migration was supported by the 87Sr/86Sr ratio in veins and wall rocks.
  • The Palaeozoic sedimentary sequence of the Prague synform (Ordovician- Devonian) in the centre of the Bohemian massif underwent Variscan deformation and thermal overprint events. Variscan veins widespread throughout the sedimentary strata have precipitated from syntectonic aqueous and hydrocarbon-rich fluids. Homogenization temperatures of aqueous inclusions increased from 70 up to 226 degC in the Cambrian rocks underlying the Prague synform. Seawater, modified due to intensive water-rock interaction, was the main fluid component. Fluid flow was limited and restricted to the lithostratigraphic compartments forming a rock-buffered system. Stable isotopic modelling (C, O) and final interpretations of the confined hydrostratigraphic fluid migration was supported by the 87Sr/86Sr ratio in veins and wall rocks. (en)
Title
  • Litho-stratigraphic effect on Variscan fluid flow within the Prague synform, Barrandian: Evidence based on C, O, Sr isotopes and fluid inclusions
  • Litho-stratigraphic effect on Variscan fluid flow within the Prague synform, Barrandian: Evidence based on C, O, Sr isotopes and fluid inclusions (en)
skos:prefLabel
  • Litho-stratigraphic effect on Variscan fluid flow within the Prague synform, Barrandian: Evidence based on C, O, Sr isotopes and fluid inclusions
  • Litho-stratigraphic effect on Variscan fluid flow within the Prague synform, Barrandian: Evidence based on C, O, Sr isotopes and fluid inclusions (en)
skos:notation
  • RIV/00216224:14310/12:00057087!RIV13-AV0-14310___
http://linked.open...avai/riv/aktivita
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  • P(IAA3013406), Z(MSM0021622412)
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  • 1
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  • 147255
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  • RIV/00216224:14310/12:00057087
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  • Bohemian Massif; Palaeozoic; Variscan orogeny; veins; fluid inclusions; stable isotopes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
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  • [D4F9FE03FA4A]
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  • Marine and Petroleum Geology
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  • 35
http://linked.open...iv/tvurceVysledku
  • Melichar, Rostislav
  • Slobodník, Marek
  • Bakker, Ronald
  • Hurai, Vratislav
http://linked.open...ain/vavai/riv/wos
  • 000305917500010
http://linked.open...n/vavai/riv/zamer
issn
  • 0264-8172
number of pages
http://bibframe.org/vocab/doi
  • 10.1016/j.marpetgeo.2012.01.003
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  • 14310
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