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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F01%3A09013119%21RIV%2F2003%2FAV0%2FA09003%2FN
rdf:type
n8:Vysledek skos:Concept
dcterms: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.
dcterms: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?
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?
skos:notation
RIV/67985831:_____/01:09013119!RIV/2003/AV0/A09003/N
n3:strany
111;114
n3:aktivita
n6:Z n6:P
n3:aktivity
P(KSK3012103), Z(AV0Z3013912)
n3:cisloPeriodika
N/A
n3:dodaniDat
n17:2003
n3:domaciTvurceVysledku
n16:8642702
n3:druhVysledku
n10:J
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n5:predkladatel
n3:idSjednocenehoVysledku
681127
n3:idVysledku
RIV/67985831:_____/01:09013119
n3:jazykVysledku
n14:eng
n3:klicovaSlova
Geochemistry; tectonic setting; Srbsko Formation of the Barrandian area
n3:klicoveSlovo
n7:Geochemistry n7:tectonic%20setting n7:Srbsko%20Formation%20of%20the%20Barrandian%20area
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[52929A1D0090]
n3:nazevZdroje
Geolines
n3:obor
n15:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
2
n3:pocetUcastnikuAkce
0
n3:pocetZahranicnichUcastnikuAkce
0
n3:projekt
n4:KSK3012103
n3:rokUplatneniVysledku
n17:2001
n3:svazekPeriodika
13
n3:tvurceVysledku
Hladil, Jindřich Strnad, L.
n3:zamer
n12:AV0Z3013912
s:issn
1210-9606
s:numberOfPages
4