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rdf:type
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Description
| - An extreme sedimentary starving combined with dissolution characterises the Kačák Member, which covers the limestones of depths of several hundreds of meters. The siliciclastic sediments of Srbsko Fm. contained pelagic carbonate ooze, which was significantly dissolved. Distal turbiditite siltstones/sandstones of Roblín Member contain, beside quartz, also small lithic and feldspar grains. The TM contain garnet and zircon, pyroxene, tourmaline, apatite, Fe-Ti oxides, spinel, Fe-sulphides, and rarely Mg-olivine and Mg-biotite. Long prismatic, dipyramidal and oval zircons were found. The least mobile elements were used for tectonic-setting proxies (e.g., La-Sc-Th, Th-Sc-Zr/10 or Th-Co-Zr/10), where CIA-ACM settings were indicated. The pull-down of the seafloor into the abyss was followed by shedding of continental material, then, the tectonic thickening and shallowing suggest formation of accretionary prism.
- An extreme sedimentary starving combined with dissolution characterises the Kačák Member, which covers the limestones of depths of several hundreds of meters. The siliciclastic sediments of Srbsko Fm. contained pelagic carbonate ooze, which was significantly dissolved. Distal turbiditite siltstones/sandstones of Roblín Member contain, beside quartz, also small lithic and feldspar grains. The TM contain garnet and zircon, pyroxene, tourmaline, apatite, Fe-Ti oxides, spinel, Fe-sulphides, and rarely Mg-olivine and Mg-biotite. Long prismatic, dipyramidal and oval zircons were found. The least mobile elements were used for tectonic-setting proxies (e.g., La-Sc-Th, Th-Sc-Zr/10 or Th-Co-Zr/10), where CIA-ACM settings were indicated. The pull-down of the seafloor into the abyss was followed by shedding of continental material, then, the tectonic thickening and shallowing suggest formation of accretionary prism. (en)
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Title
| - Geochemistry and composition of the Middle Devonian Srbsko Formation in Barrandian Area, Bohemian Massif: A trench or fore-arc strike-slip basin fill with material from volcanic arc of continental margin?
- Geochemistry and composition of the Middle Devonian Srbsko Formation in Barrandian Area, Bohemian Massif: A trench or fore-arc strike-slip basin fill with material from volcanic arc of continental margin? (en)
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skos:prefLabel
| - Geochemistry and composition of the Middle Devonian Srbsko Formation in Barrandian Area, Bohemian Massif: A trench or fore-arc strike-slip basin fill with material from volcanic arc of continental margin?
- Geochemistry and composition of the Middle Devonian Srbsko Formation in Barrandian Area, Bohemian Massif: A trench or fore-arc strike-slip basin fill with material from volcanic arc of continental margin? (en)
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skos:notation
| - RIV/67985831:_____/01:09013119!RIV/2003/AV0/A09003/N
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http://linked.open.../vavai/riv/strany
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
| - P(KSK3012103), Z(AV0Z3013912)
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/67985831:_____/01:09013119
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Geochemistry; tectonic setting; Srbsko Formation of the Barrandian area (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...ocetUcastnikuAkce
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http://linked.open...nichUcastnikuAkce
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Hladil, Jindřich
- Strnad, L.
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http://linked.open...n/vavai/riv/zamer
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issn
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number of pages
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