Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

Kjetil Indrevær; Sebastien Gac; Roy H. Gabrielsen; Jan Inge Faleide

doi:10.1144/jgs2017-063

Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

View ORCID ProfileKjetil Indrevær, Sebastien Gac, View ORCID ProfileRoy H. Gabrielsen and View ORCID ProfileJan Inge Faleide

Journal of the Geological Society, 175, 497-508, 14 December 2017, https://doi.org/10.1144/jgs2017-063

Kjetil Indrevær

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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ORCID record for Kjetil Indrevær
For correspondence: kjetil.indrevar@geo.uio.no

Sebastien Gac

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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Roy H. Gabrielsen

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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ORCID record for Roy H. Gabrielsen

Jan Inge Faleide

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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ORCID record for Jan Inge Faleide

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DOI

https://doi.org/10.1144/jgs2017-063

Published By

Geological Society of London

Print ISSN

0016-7649

Online ISSN

2041-479X

History

Received 15 May 2017
Revision received 19 August 2017
Accepted 7 November 2017
Published 14 December 2017.

Author Information

Kjetil Indrevær*,
Sebastien Gac,
Roy H. Gabrielsen and
Jan Inge Faleide

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

↵*Correspondence: kjetil.indrevar{at}geo.uio.no

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Funding

Research Council of Norway
228107

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Journal of the Geological Society

Volume 175, Issue 3

May 2018

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Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

Kjetil Indrevær, Sebastien Gac, Roy H. Gabrielsen and Jan Inge Faleide

Journal of the Geological Society, 175, 497-508, 14 December 2017, https://doi.org/10.1144/jgs2017-063

Kjetil Indrevær

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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ORCID record for Kjetil Indrevær
For correspondence: kjetil.indrevar@geo.uio.no

Sebastien Gac

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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Roy H. Gabrielsen

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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ORCID record for Roy H. Gabrielsen

Jan Inge Faleide

The Research Centre for Arctic Petroleum Exploration (ARCEx), Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0371 Oslo, Norway

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ORCID record for Jan Inge Faleide

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Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

Kjetil Indrevær, Sebastien Gac, Roy H. Gabrielsen and Jan Inge Faleide

Journal of the Geological Society, 175, 497-508, 14 December 2017, https://doi.org/10.1144/jgs2017-063

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Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

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Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

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Crustal-scale subsidence and uplift caused by metamorphic phase changes in the lower crust: a model for the evolution of the Loppa High area, SW Barents Sea from late Paleozoic to Present

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