Synchronous oceanic spreading and continental rifting in West Antarctica

Magnetic anomalies associated with new ocean crust formation in the Adare Basin off north-western Ross Sea (43–26 Ma) can be traced directly into the Northern Basin that underlies the adjacent morphological continental shelf, implying a continuity in the emplacement of oceanic crust. Steep gravi...

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Published in:Geophysical Research Letters
Main Authors: Davey, F. J., Granot, R., Cande, S. C., Stock, J. M., Selvans, M., Ferraccioli, F.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2016
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Online Access:https://doi.org/10.1002/2016GL069087
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spelling ftcaltechauth:oai:authors.library.caltech.edu:h2dby-zqc30 2024-09-15T17:47:58+00:00 Synchronous oceanic spreading and continental rifting in West Antarctica Davey, F. J. Granot, R. Cande, S. C. Stock, J. M. Selvans, M. Ferraccioli, F. 2016-06-28 https://doi.org/10.1002/2016GL069087 unknown American Geophysical Union https://doi.org/10.1002/2016GL069087 oai:authors.library.caltech.edu:h2dby-zqc30 eprintid:70364 resolverid:CaltechAUTHORS:20160915-090411864 info:eu-repo/semantics/openAccess Other Geophysical Research Letters, 43(12), 6162-6169, (2016-06-28) continental rifting info:eu-repo/semantics/article 2016 ftcaltechauth https://doi.org/10.1002/2016GL069087 2024-08-06T15:35:04Z Magnetic anomalies associated with new ocean crust formation in the Adare Basin off north-western Ross Sea (43–26 Ma) can be traced directly into the Northern Basin that underlies the adjacent morphological continental shelf, implying a continuity in the emplacement of oceanic crust. Steep gravity gradients along the margins of the Northern Basin, particularly in the east, suggest that little extension and thinning of continental crust occurred before it ruptured and the new oceanic crust formed, unlike most other continental rifts and the Victoria Land Basin further south. A preexisting weak crust and localization of strain by strike-slip faulting are proposed as the factors allowing the rapid rupture of continental crust. © 2016. American Geophysical Union. Received 11 APR 2016; Accepted 31 MAY 2016; Accepted article online 3 JUN 2016; Published online 21 JUN 2016. The aeromagnetic map in Figure 2 is available from F.F. and will be submitted to the NERC/BAS Polar Data Centre. Magnetic anomaly picks have been submitted to The Global Seafloor Fabric and Magnetic Lineation Data Base Project, link: http://www.soest.hawaii.edu/PT/GSFML/ML/index.html. The marine gravity data are available from GeoMap App, cruise NBP0701. The seismic data of Brancolini et al., 1995 are also available from the SCAR seismic Data Library System—http://sdls.ogs.trieste.it/. Sonobuoy data from NBP0701 are available from http://web.gps.caltech.edu/~clay/Adare_Sonobuoy/Adare_Sonobuoy.html). Adare Basin Sonobuoy data (2007), Sonobuoy Data from the Adare Basin, Antarctica. Caltech. Dataset. doi:10.7909/C37P8W9P. S.C. acknowledges funding from NSF grant OPP04-40959 and F.D. for funding from NZGSF. We acknowledge the critical reviews by John Behrendt and two anonymous reviewers that has greatly improved the paper. F.D. thanks Susan Ellis for advice. Published - Davey_et_al-2016-Geophysical_Research_Letters.pdf Supplemental Material - grl54560-sup-0001-SuppInfo.doc Article in Journal/Newspaper Antarc* Antarctica Ross Sea Victoria Land West Antarctica Caltech Authors (California Institute of Technology) Geophysical Research Letters 43 12 6162 6169
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic continental rifting
spellingShingle continental rifting
Davey, F. J.
Granot, R.
Cande, S. C.
Stock, J. M.
Selvans, M.
Ferraccioli, F.
Synchronous oceanic spreading and continental rifting in West Antarctica
topic_facet continental rifting
description Magnetic anomalies associated with new ocean crust formation in the Adare Basin off north-western Ross Sea (43–26 Ma) can be traced directly into the Northern Basin that underlies the adjacent morphological continental shelf, implying a continuity in the emplacement of oceanic crust. Steep gravity gradients along the margins of the Northern Basin, particularly in the east, suggest that little extension and thinning of continental crust occurred before it ruptured and the new oceanic crust formed, unlike most other continental rifts and the Victoria Land Basin further south. A preexisting weak crust and localization of strain by strike-slip faulting are proposed as the factors allowing the rapid rupture of continental crust. © 2016. American Geophysical Union. Received 11 APR 2016; Accepted 31 MAY 2016; Accepted article online 3 JUN 2016; Published online 21 JUN 2016. The aeromagnetic map in Figure 2 is available from F.F. and will be submitted to the NERC/BAS Polar Data Centre. Magnetic anomaly picks have been submitted to The Global Seafloor Fabric and Magnetic Lineation Data Base Project, link: http://www.soest.hawaii.edu/PT/GSFML/ML/index.html. The marine gravity data are available from GeoMap App, cruise NBP0701. The seismic data of Brancolini et al., 1995 are also available from the SCAR seismic Data Library System—http://sdls.ogs.trieste.it/. Sonobuoy data from NBP0701 are available from http://web.gps.caltech.edu/~clay/Adare_Sonobuoy/Adare_Sonobuoy.html). Adare Basin Sonobuoy data (2007), Sonobuoy Data from the Adare Basin, Antarctica. Caltech. Dataset. doi:10.7909/C37P8W9P. S.C. acknowledges funding from NSF grant OPP04-40959 and F.D. for funding from NZGSF. We acknowledge the critical reviews by John Behrendt and two anonymous reviewers that has greatly improved the paper. F.D. thanks Susan Ellis for advice. Published - Davey_et_al-2016-Geophysical_Research_Letters.pdf Supplemental Material - grl54560-sup-0001-SuppInfo.doc
format Article in Journal/Newspaper
author Davey, F. J.
Granot, R.
Cande, S. C.
Stock, J. M.
Selvans, M.
Ferraccioli, F.
author_facet Davey, F. J.
Granot, R.
Cande, S. C.
Stock, J. M.
Selvans, M.
Ferraccioli, F.
author_sort Davey, F. J.
title Synchronous oceanic spreading and continental rifting in West Antarctica
title_short Synchronous oceanic spreading and continental rifting in West Antarctica
title_full Synchronous oceanic spreading and continental rifting in West Antarctica
title_fullStr Synchronous oceanic spreading and continental rifting in West Antarctica
title_full_unstemmed Synchronous oceanic spreading and continental rifting in West Antarctica
title_sort synchronous oceanic spreading and continental rifting in west antarctica
publisher American Geophysical Union
publishDate 2016
url https://doi.org/10.1002/2016GL069087
genre Antarc*
Antarctica
Ross Sea
Victoria Land
West Antarctica
genre_facet Antarc*
Antarctica
Ross Sea
Victoria Land
West Antarctica
op_source Geophysical Research Letters, 43(12), 6162-6169, (2016-06-28)
op_relation https://doi.org/10.1002/2016GL069087
oai:authors.library.caltech.edu:h2dby-zqc30
eprintid:70364
resolverid:CaltechAUTHORS:20160915-090411864
op_rights info:eu-repo/semantics/openAccess
Other
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container_title Geophysical Research Letters
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container_issue 12
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