New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data

Insights into the spreading evolution of the Knipovich Ridge and development of the Fram Strait are revealed from a recent aeromagnetic survey. As an ultraslow spreading ridge in an oblique system located between the Svalbard–Barents Sea and the Northeast Greenland rifted margins, the dynamics of th...

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Published in:Geophysical Journal International
Main Authors: Dumais, Marie-Andrée, Gernigon, Laurent, Olesen, Odleiv, Johansen, Ståle Emil, Brönner, Marco
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press 2021
Subjects:
Online Access:https://hdl.handle.net/11250/2977570
https://doi.org/10.1093/gji/ggaa527
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author Dumais, Marie-Andrée
Gernigon, Laurent
Olesen, Odleiv
Johansen, Ståle Emil
Brönner, Marco
author_facet Dumais, Marie-Andrée
Gernigon, Laurent
Olesen, Odleiv
Johansen, Ståle Emil
Brönner, Marco
author_sort Dumais, Marie-Andrée
collection NTNU Open Archive (Norwegian University of Science and Technology)
container_issue 2
container_start_page 1422
container_title Geophysical Journal International
container_volume 224
description Insights into the spreading evolution of the Knipovich Ridge and development of the Fram Strait are revealed from a recent aeromagnetic survey. As an ultraslow spreading ridge in an oblique system located between the Svalbard–Barents Sea and the Northeast Greenland rifted margins, the dynamics of the Knipovich Ridge opening has long been debated. Its 90° bend with the Mohns Ridge, rare in plate tectonics, affects the evolution of the Fram Strait and motivates the study of crustal deformation with this distinctive configuration. We identified magnetic isochrons on either side of the present-day Knipovich Ridge. These magnetic observations considerably reduce the mapped extent of the oceanic domain and question the present understanding of the conjugate rifted margins. Our analysis reveals a failed spreading system before a major spreading reorganization of the Fram Strait gateway around magnetic chron C6 (circa 20 Ma). publishedVersion
format Article in Journal/Newspaper
genre Barents Sea
Fram Strait
Greenland
Svalbard
genre_facet Barents Sea
Fram Strait
Greenland
Svalbard
geographic Barents Sea
Greenland
Knipovich Ridge
Svalbard
geographic_facet Barents Sea
Greenland
Knipovich Ridge
Svalbard
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institution Open Polar
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op_doi https://doi.org/10.1093/gji/ggaa527
op_relation Geophysical Journal International. 2021, 224 (2), 1422-1428.
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https://hdl.handle.net/11250/2977570
https://doi.org/10.1093/gji/ggaa527
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op_rights Navngivelse 4.0 Internasjonal
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spelling ftntnutrondheimi:oai:ntnuopen.ntnu.no:11250/2977570 2025-01-16T21:11:47+00:00 New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data Dumais, Marie-Andrée Gernigon, Laurent Olesen, Odleiv Johansen, Ståle Emil Brönner, Marco 2021 application/pdf https://hdl.handle.net/11250/2977570 https://doi.org/10.1093/gji/ggaa527 eng eng Oxford University Press Geophysical Journal International. 2021, 224 (2), 1422-1428. urn:issn:0956-540X https://hdl.handle.net/11250/2977570 https://doi.org/10.1093/gji/ggaa527 cristin:1870847 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 1422-1428 224 Geophysical Journal International 2 Peer reviewed Journal article 2021 ftntnutrondheimi https://doi.org/10.1093/gji/ggaa527 2022-02-09T23:38:20Z Insights into the spreading evolution of the Knipovich Ridge and development of the Fram Strait are revealed from a recent aeromagnetic survey. As an ultraslow spreading ridge in an oblique system located between the Svalbard–Barents Sea and the Northeast Greenland rifted margins, the dynamics of the Knipovich Ridge opening has long been debated. Its 90° bend with the Mohns Ridge, rare in plate tectonics, affects the evolution of the Fram Strait and motivates the study of crustal deformation with this distinctive configuration. We identified magnetic isochrons on either side of the present-day Knipovich Ridge. These magnetic observations considerably reduce the mapped extent of the oceanic domain and question the present understanding of the conjugate rifted margins. Our analysis reveals a failed spreading system before a major spreading reorganization of the Fram Strait gateway around magnetic chron C6 (circa 20 Ma). publishedVersion Article in Journal/Newspaper Barents Sea Fram Strait Greenland Svalbard NTNU Open Archive (Norwegian University of Science and Technology) Barents Sea Greenland Knipovich Ridge ENVELOPE(7.074,7.074,75.712,75.712) Svalbard Geophysical Journal International 224 2 1422 1428
spellingShingle Dumais, Marie-Andrée
Gernigon, Laurent
Olesen, Odleiv
Johansen, Ståle Emil
Brönner, Marco
New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data
title New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data
title_full New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data
title_fullStr New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data
title_full_unstemmed New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data
title_short New interpretation of the spreading evolution of the Knipovich Ridge derived from aeromagnetic data
title_sort new interpretation of the spreading evolution of the knipovich ridge derived from aeromagnetic data
url https://hdl.handle.net/11250/2977570
https://doi.org/10.1093/gji/ggaa527