Počet záznamů: 1  

Provenance of Neoproterozoic to upper Cretaceous sedimentary rocks, eastern Greenland: Implications for recognizing the sources of sediments in the Norwegian Sea

  1. 1.
    SYSNO ASEP0361338
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevProvenance of Neoproterozoic to upper Cretaceous sedimentary rocks, eastern Greenland: Implications for recognizing the sources of sediments in the Norwegian Sea
    Tvůrce(i) Sláma, Jiří (GLU-S) SAI, RID, ORCID
    Walderhaug, O. (NO)
    Fonneland, H. (NO)
    Kosler, J. (NO)
    Pederson, R. B. (NO)
    Zdroj.dok.Sedimentary geology. - : Elsevier - ISSN 0037-0738
    Roč. 238, 3/4 (2011), s. 254-267
    Poč.str.14 s.
    Forma vydáníWWW - WWW
    Jazyk dok.eng - angličtina
    Země vyd.NL - Nizozemsko
    Klíč. slovasedimentary ; Eastern Greenland ; provenance ; U-Pb and Lu-Hf ; zircon ; Jan Mayen Island ; North Atlantic
    Vědní obor RIVDB - Geologie a mineralogie
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000293205700003
    EID SCOPUS79959576380
    DOI10.1016/j.sedgeo.2011.04.018
    AnotaceDetrital 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.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2012
Počet záznamů: 1  

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