Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ...
Geophysical data acquired using R/V Polarstern constrain the structure and age of the rifted oceanic margin of West Antarctica. West of the Antipodes Fracture Zone, the 145 km wide continent-ocean transition zone (COTZ) of the Marie Byrd Land sector resembles a typical magma-poor margin. New gravity...
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ftdatacite:10.1594/pangaea.858217 2024-09-15T17:39:09+00:00 Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... Wobbe, Florian Gohl, Karsten Chambord, A Sutherland, R 2012 application/zip https://dx.doi.org/10.1594/pangaea.858217 https://doi.pangaea.de/10.1594/PANGAEA.858217 en eng PANGAEA https://dx.doi.org/10.1029/2011gc003742 Creative Commons Attribution Non Commercial Share Alike 3.0 Unported https://creativecommons.org/licenses/by-nc-sa/3.0/legalcode cc-by-nc-sa-3.0 Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.85821710.1029/2011gc003742 2024-08-01T11:01:20Z Geophysical data acquired using R/V Polarstern constrain the structure and age of the rifted oceanic margin of West Antarctica. West of the Antipodes Fracture Zone, the 145 km wide continent-ocean transition zone (COTZ) of the Marie Byrd Land sector resembles a typical magma-poor margin. New gravity and seismic reflection data indicates initial continental crust of thickness 24 km, that was stretched 90 km. Farther east, the Bellingshausen sector is broad and complex with abundant evidence for volcanism, the COTZ is ~670 km wide, and the nature of crust within the COTZ is uncertain. Margin extension is estimated to be 106-304 km in this sector. Seafloor magnetic anomalies adjacent to Marie Byrd Land near the Pahemo Fracture Zone indicate full-spreading rate during c33-c31 (80-68 Myr) of 60 mm/yr, increasing to 74 mm/yr at c27 (62 Myr), and then dropping to 22 mm/yr by c22 (50 Myr). Spreading rates were lower to the west. Extrapolation towards the continental margin indicates initial oceanic crust formation ... : Data was extracted from the supplementary zip file provided with the article. ... Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctica Marie Byrd Land Sea ice West Antarctica DataCite |
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Open Polar |
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DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Wobbe, Florian Gohl, Karsten Chambord, A Sutherland, R Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... |
topic_facet |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
Geophysical data acquired using R/V Polarstern constrain the structure and age of the rifted oceanic margin of West Antarctica. West of the Antipodes Fracture Zone, the 145 km wide continent-ocean transition zone (COTZ) of the Marie Byrd Land sector resembles a typical magma-poor margin. New gravity and seismic reflection data indicates initial continental crust of thickness 24 km, that was stretched 90 km. Farther east, the Bellingshausen sector is broad and complex with abundant evidence for volcanism, the COTZ is ~670 km wide, and the nature of crust within the COTZ is uncertain. Margin extension is estimated to be 106-304 km in this sector. Seafloor magnetic anomalies adjacent to Marie Byrd Land near the Pahemo Fracture Zone indicate full-spreading rate during c33-c31 (80-68 Myr) of 60 mm/yr, increasing to 74 mm/yr at c27 (62 Myr), and then dropping to 22 mm/yr by c22 (50 Myr). Spreading rates were lower to the west. Extrapolation towards the continental margin indicates initial oceanic crust formation ... : Data was extracted from the supplementary zip file provided with the article. ... |
format |
Article in Journal/Newspaper |
author |
Wobbe, Florian Gohl, Karsten Chambord, A Sutherland, R |
author_facet |
Wobbe, Florian Gohl, Karsten Chambord, A Sutherland, R |
author_sort |
Wobbe, Florian |
title |
Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... |
title_short |
Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... |
title_full |
Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... |
title_fullStr |
Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... |
title_full_unstemmed |
Seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from New Zealand to the Amundsen Sea (south of 64°S) ... |
title_sort |
seafloor magnetic anomalies and ages observed from shipboard and airborne measurements from new zealand to the amundsen sea (south of 64°s) ... |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.858217 https://doi.pangaea.de/10.1594/PANGAEA.858217 |
genre |
Amundsen Sea Antarc* Antarctic Antarctica Marie Byrd Land Sea ice West Antarctica |
genre_facet |
Amundsen Sea Antarc* Antarctic Antarctica Marie Byrd Land Sea ice West Antarctica |
op_relation |
https://dx.doi.org/10.1029/2011gc003742 |
op_rights |
Creative Commons Attribution Non Commercial Share Alike 3.0 Unported https://creativecommons.org/licenses/by-nc-sa/3.0/legalcode cc-by-nc-sa-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.85821710.1029/2011gc003742 |
_version_ |
1810477788694577152 |