IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications

The opening of the North Atlantic about 56 My ago was associated with the emplacement of the North Atlantic Igneous Province, including the deposition of voluminous extrusive basaltic successions and intrusion of magma into the surrounding sedimentary basins. The mid-Norwegian Margin is a global typ...

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Main Authors: Planke, Sverre, Berndt, Christian, Alvarez Zarikian, Carlos A., the Expedition 396 Scientists
Other Authors: Marine Palynology, Marine palynology and palaeoceanography
Format: Report
Language:English
Published: International Ocean Discovery Program (IODP) 2022
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/425670
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spelling ftunivutrecht:oai:dspace.library.uu.nl:1874/425670 2023-11-12T04:22:00+01:00 IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications Planke, Sverre Berndt, Christian Alvarez Zarikian, Carlos A. the Expedition 396 Scientists Marine Palynology Marine palynology and palaeoceanography 2022 application/pdf https://dspace.library.uu.nl/handle/1874/425670 en eng International Ocean Discovery Program (IODP) https://dspace.library.uu.nl/handle/1874/425670 info:eu-repo/semantics/OpenAccess Oceanography Report 2022 ftunivutrecht 2023-11-01T23:29:42Z The opening of the North Atlantic about 56 My ago was associated with the emplacement of the North Atlantic Igneous Province, including the deposition of voluminous extrusive basaltic successions and intrusion of magma into the surrounding sedimentary basins. The mid-Norwegian Margin is a global type example of such volcanic rifted margins and is well suited for scientific drilling with its thin sediment cover and good data coverage. During International Ocean Discovery Program Expedition 396, 21 boreholes were drilled at 10 sites in five different geological settings on this volcanic margin. The boreholes sampled a multitude of igneous and sedimentary settings ranging from lava flow fields to hydrothermal vent complexes, along with thick successions of upper Paleocene and lower Eocene strata. A comprehensive suite of wireline logs was collected in eight boreholes. The main goals of the expedition were to provide constraints for geodynamic models to test different hypotheses that can explain the rapid emplacement of large igneous provinces and the hypothesis that the associated Paleocene/Eocene Thermal Maximum was caused by hydrothermal release of carbon in response to magmatic intrusions. Successful drilling, combined with high core recovery of target intervals of all nine primary sites and one additional alternate site, should allow us to achieve these goals during postcruise work. Report North Atlantic Utrecht University Repository
institution Open Polar
collection Utrecht University Repository
op_collection_id ftunivutrecht
language English
topic Oceanography
spellingShingle Oceanography
Planke, Sverre
Berndt, Christian
Alvarez Zarikian, Carlos A.
the Expedition 396 Scientists
IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications
topic_facet Oceanography
description The opening of the North Atlantic about 56 My ago was associated with the emplacement of the North Atlantic Igneous Province, including the deposition of voluminous extrusive basaltic successions and intrusion of magma into the surrounding sedimentary basins. The mid-Norwegian Margin is a global type example of such volcanic rifted margins and is well suited for scientific drilling with its thin sediment cover and good data coverage. During International Ocean Discovery Program Expedition 396, 21 boreholes were drilled at 10 sites in five different geological settings on this volcanic margin. The boreholes sampled a multitude of igneous and sedimentary settings ranging from lava flow fields to hydrothermal vent complexes, along with thick successions of upper Paleocene and lower Eocene strata. A comprehensive suite of wireline logs was collected in eight boreholes. The main goals of the expedition were to provide constraints for geodynamic models to test different hypotheses that can explain the rapid emplacement of large igneous provinces and the hypothesis that the associated Paleocene/Eocene Thermal Maximum was caused by hydrothermal release of carbon in response to magmatic intrusions. Successful drilling, combined with high core recovery of target intervals of all nine primary sites and one additional alternate site, should allow us to achieve these goals during postcruise work.
author2 Marine Palynology
Marine palynology and palaeoceanography
format Report
author Planke, Sverre
Berndt, Christian
Alvarez Zarikian, Carlos A.
the Expedition 396 Scientists
author_facet Planke, Sverre
Berndt, Christian
Alvarez Zarikian, Carlos A.
the Expedition 396 Scientists
author_sort Planke, Sverre
title IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications
title_short IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications
title_full IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications
title_fullStr IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications
title_full_unstemmed IODP Expedition 396 Preliminary Report: Mid-Norwegian Margin Magmatism and Paleoclimate Implications
title_sort iodp expedition 396 preliminary report: mid-norwegian margin magmatism and paleoclimate implications
publisher International Ocean Discovery Program (IODP)
publishDate 2022
url https://dspace.library.uu.nl/handle/1874/425670
genre North Atlantic
genre_facet North Atlantic
op_relation https://dspace.library.uu.nl/handle/1874/425670
op_rights info:eu-repo/semantics/OpenAccess
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