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LARSEN, LOTTE M., PEDERSEN, ASGER K., TEGNER, CHRISTIAN, DUNCAN, ROBERT A., HALD, NIELS, LARSEN, JØRGEN G. (2016) Age of Tertiary volcanic rocks on the West Greenland continental margin: volcanic evolution and event correlation to other parts of the North Atlantic Igneous Province. Geological Magazine, 153 (3) 487-511 doi:10.1017/s0016756815000515

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Reference TypeJournal (article/letter/editorial)
TitleAge of Tertiary volcanic rocks on the West Greenland continental margin: volcanic evolution and event correlation to other parts of the North Atlantic Igneous Province
JournalGeological Magazine
AuthorsLARSEN, LOTTE M.Author
PEDERSEN, ASGER K.Author
TEGNER, CHRISTIANAuthor
DUNCAN, ROBERT A.Author
HALD, NIELSAuthor
LARSEN, JØRGEN G.Author
Year2016 (May)Volume153
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756815000515Search in ResearchGate
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Mindat Ref. ID261034Long-form Identifiermindat:1:5:261034:8
GUID0
Full ReferenceLARSEN, LOTTE M., PEDERSEN, ASGER K., TEGNER, CHRISTIAN, DUNCAN, ROBERT A., HALD, NIELS, LARSEN, JØRGEN G. (2016) Age of Tertiary volcanic rocks on the West Greenland continental margin: volcanic evolution and event correlation to other parts of the North Atlantic Igneous Province. Geological Magazine, 153 (3) 487-511 doi:10.1017/s0016756815000515
Plain TextLARSEN, LOTTE M., PEDERSEN, ASGER K., TEGNER, CHRISTIAN, DUNCAN, ROBERT A., HALD, NIELS, LARSEN, JØRGEN G. (2016) Age of Tertiary volcanic rocks on the West Greenland continental margin: volcanic evolution and event correlation to other parts of the North Atlantic Igneous Province. Geological Magazine, 153 (3) 487-511 doi:10.1017/s0016756815000515
In(2016, May) Geological Magazine Vol. 153 (3) Cambridge University Press (CUP)
Abstract/NotesAbstractRadiometric ages for undated parts of the volcanic succession and intrusions in West Greenland were obtained by the 40Ar–39Ar incremental heating method. Acceptable crystallization ages were obtained for 27 samples. Combined with published results the new data provide a volcanic stratigraphy correlatable throughout the Nuussuaq Basin. The thick onshore volcanic pile consists of four widespread formations: 62.5–61 Ma picrites (Vaigat Formation), 61–60 Ma depleted basalts (Maligât Formation and the Hellefisk-1 well), 60–58 Ma less-depleted basalts (Svartenhuk Formation) and 56–54 Ma enriched basalts (Naqerloq Formation). Two local successions comprise 53.5 Ma alkali basalts (Erqua Formation) and 38.7 Ma transitional basalts (Talerua Member). A central volcano developed on Ubekendt Ejland, leading to the Sarqâta qáqâ gabbro-granophyre intrusion at 57–55 Ma. Pre-break-up volcanism took place further south as early as 64–63 Ma. The offshore volcanic succession most probably comprises the known onshore succession plus some younger lavas. The change in spreading direction near the Paleocene–Eocene boundary took place west of the Nuussuaq Basin c. 56.2 Ma. Some tectonomagmatic events are correlatable across the entire North Atlantic Igneous Province. A quiescent 58–56 Ma period correlates with similar periods in East Greenland and the Faroes, and the Naqerloq Formation is coeval with the Eocene basalts in East Greenland. The Paleocene and Eocene tholeiitic basalts are distinguishable chemically; in early Eocene time, mantle typical of the Iceland plume seems to have extended beneath the whole West Greenland margin as well as the central East Greenland margin.


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