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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F11%3A00361338%21RIV12-AV0-67985831
rdf:type
n14:Vysledek skos:Concept
dcterms:description
Detrital zircon U–Pb and Lu–Hf isotope data from Neoproterozoic to Cretaceous sandstones exposed in eastern Greenland, 70°30–74°N, are reported to characterize and evaluate the provenance from Greenland during pre-breakup and post-breakup sedimentation in the Norwegian–Greenland Sea. Middle Devonian to Lower Cretaceous samples all show similar detrital zircon age distributions characterized by variable Archean populations, abundant Proterozoic populations ranging from ca. 2000 to 900 Ma and a Caledonian population peaking at ca. 440 Ma. Neoproterozoic sediments of the Eleonore Bay Supergroup give a more narrow age distribution with a dominant age peak at 1100 to 1000 Ma, a secondary peak at 1700–1400 Ma, and rare Archean to Paleoproterozoic ages. The scarcity of Archean zircons could indicate a rather limited role of the Archean basement rocks of the eastern Greenland Caledonian orogenic belt as a source for some of the analyzed younger sedimentary rocks. Detrital zircon U–Pb and Lu–Hf isotope data from Neoproterozoic to Cretaceous sandstones exposed in eastern Greenland, 70°30–74°N, are reported to characterize and evaluate the provenance from Greenland during pre-breakup and post-breakup sedimentation in the Norwegian–Greenland Sea. Middle Devonian to Lower Cretaceous samples all show similar detrital zircon age distributions characterized by variable Archean populations, abundant Proterozoic populations ranging from ca. 2000 to 900 Ma and a Caledonian population peaking at ca. 440 Ma. Neoproterozoic sediments of the Eleonore Bay Supergroup give a more narrow age distribution with a dominant age peak at 1100 to 1000 Ma, a secondary peak at 1700–1400 Ma, and rare Archean to Paleoproterozoic ages. The scarcity of Archean zircons could indicate a rather limited role of the Archean basement rocks of the eastern Greenland Caledonian orogenic belt as a source for some of the analyzed younger sedimentary rocks.
dcterms:title
Provenance of Neoproterozoic to upper Cretaceous sedimentary rocks, eastern Greenland: Implications for recognizing the sources of sediments in the Norwegian Sea Provenance of Neoproterozoic to upper Cretaceous sedimentary rocks, eastern Greenland: Implications for recognizing the sources of sediments in the Norwegian Sea
skos:prefLabel
Provenance of Neoproterozoic to upper Cretaceous sedimentary rocks, eastern Greenland: Implications for recognizing the sources of sediments in the Norwegian Sea Provenance of Neoproterozoic to upper Cretaceous sedimentary rocks, eastern Greenland: Implications for recognizing the sources of sediments in the Norwegian Sea
skos:notation
RIV/67985831:_____/11:00361338!RIV12-AV0-67985831
n14:predkladatel
n17:ico%3A67985831
n4:aktivita
n18:Z
n4:aktivity
Z(AV0Z30130516)
n4:cisloPeriodika
3/4
n4:dodaniDat
n6:2012
n4:domaciTvurceVysledku
n11:4026772
n4:druhVysledku
n12:J
n4:duvernostUdaju
n16:S
n4:entitaPredkladatele
n19:predkladatel
n4:idSjednocenehoVysledku
224929
n4:idVysledku
RIV/67985831:_____/11:00361338
n4:jazykVysledku
n7:eng
n4:klicovaSlova
sedimentary; Eastern Greenland; provenance; U-Pb and Lu-Hf; zircon; Jan Mayen Island; North Atlantic
n4:klicoveSlovo
n5:sedimentary n5:North%20Atlantic n5:Jan%20Mayen%20Island n5:zircon n5:U-Pb%20and%20Lu-Hf n5:Eastern%20Greenland n5:provenance
n4:kodStatuVydavatele
NL - Nizozemsko
n4:kontrolniKodProRIV
[6306DE896504]
n4:nazevZdroje
Sedimentary geology
n4:obor
n8:DB
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
5
n4:rokUplatneniVysledku
n6:2011
n4:svazekPeriodika
238
n4:tvurceVysledku
Walderhaug, O. Sláma, Jiří Kosler, J. Pederson, R. B. Fonneland, H.
n4:wos
000293205700003
n4:zamer
n15:AV0Z30130516
s:issn
0037-0738
s:numberOfPages
14
n10:doi
10.1016/j.sedgeo.2011.04.018