Uplift of the central transantarctic mountains
The Transantarctic Mountains (TAM) are the world’s longest rift shoulder but the source of their high elevation is enigmatic. To discriminate the importance of mechanical vs. thermal sources of support, a 550 km-long transect of magnetotelluric geophysical soundings spanning the central TAM was acqu...
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ftpubmed:oai:pubmedcentral.nih.gov:5693935 2023-05-15T13:40:24+02:00 Uplift of the central transantarctic mountains Wannamaker, Phil Hill, Graham Stodt, John Maris, Virginie Ogawa, Yasuo Selway, Kate Boren, Goran Bertrand, Edward Uhlmann, Daniel Ayling, Bridget Green, A. Marie Feucht, Daniel 2017-11-17 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5693935/ http://www.ncbi.nlm.nih.gov/pubmed/29150611 https://doi.org/10.1038/s41467-017-01577-2 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5693935/ http://www.ncbi.nlm.nih.gov/pubmed/29150611 http://dx.doi.org/10.1038/s41467-017-01577-2 © The Author(s) 2017 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. CC-BY Article Text 2017 ftpubmed https://doi.org/10.1038/s41467-017-01577-2 2017-11-26T01:16:12Z The Transantarctic Mountains (TAM) are the world’s longest rift shoulder but the source of their high elevation is enigmatic. To discriminate the importance of mechanical vs. thermal sources of support, a 550 km-long transect of magnetotelluric geophysical soundings spanning the central TAM was acquired. These data reveal a lithosphere of high electrical resistivity to at least 150 km depth, implying a cold stable state well into the upper mantle. Here we find that the central TAM most likely are elevated by a non-thermal, flexural cantilever mechanism which is perhaps the most clearly expressed example anywhere. West Antarctica in this region exhibits a low resistivity, moderately hydrated asthenosphere, and concentrated extension (rift necking) near the central TAM range front but with negligible thermal encroachment into the TAM. Broader scale heat flow of east-central West Antarctica appears moderate, on the order of 60–70 mW m−2, lower than that of the U.S. Great Basin. Text Antarc* Antarctica West Antarctica PubMed Central (PMC) Transantarctic Mountains West Antarctica Nature Communications 8 1 |
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Article Wannamaker, Phil Hill, Graham Stodt, John Maris, Virginie Ogawa, Yasuo Selway, Kate Boren, Goran Bertrand, Edward Uhlmann, Daniel Ayling, Bridget Green, A. Marie Feucht, Daniel Uplift of the central transantarctic mountains |
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description |
The Transantarctic Mountains (TAM) are the world’s longest rift shoulder but the source of their high elevation is enigmatic. To discriminate the importance of mechanical vs. thermal sources of support, a 550 km-long transect of magnetotelluric geophysical soundings spanning the central TAM was acquired. These data reveal a lithosphere of high electrical resistivity to at least 150 km depth, implying a cold stable state well into the upper mantle. Here we find that the central TAM most likely are elevated by a non-thermal, flexural cantilever mechanism which is perhaps the most clearly expressed example anywhere. West Antarctica in this region exhibits a low resistivity, moderately hydrated asthenosphere, and concentrated extension (rift necking) near the central TAM range front but with negligible thermal encroachment into the TAM. Broader scale heat flow of east-central West Antarctica appears moderate, on the order of 60–70 mW m−2, lower than that of the U.S. Great Basin. |
format |
Text |
author |
Wannamaker, Phil Hill, Graham Stodt, John Maris, Virginie Ogawa, Yasuo Selway, Kate Boren, Goran Bertrand, Edward Uhlmann, Daniel Ayling, Bridget Green, A. Marie Feucht, Daniel |
author_facet |
Wannamaker, Phil Hill, Graham Stodt, John Maris, Virginie Ogawa, Yasuo Selway, Kate Boren, Goran Bertrand, Edward Uhlmann, Daniel Ayling, Bridget Green, A. Marie Feucht, Daniel |
author_sort |
Wannamaker, Phil |
title |
Uplift of the central transantarctic mountains |
title_short |
Uplift of the central transantarctic mountains |
title_full |
Uplift of the central transantarctic mountains |
title_fullStr |
Uplift of the central transantarctic mountains |
title_full_unstemmed |
Uplift of the central transantarctic mountains |
title_sort |
uplift of the central transantarctic mountains |
publisher |
Nature Publishing Group UK |
publishDate |
2017 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5693935/ http://www.ncbi.nlm.nih.gov/pubmed/29150611 https://doi.org/10.1038/s41467-017-01577-2 |
geographic |
Transantarctic Mountains West Antarctica |
geographic_facet |
Transantarctic Mountains West Antarctica |
genre |
Antarc* Antarctica West Antarctica |
genre_facet |
Antarc* Antarctica West Antarctica |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5693935/ http://www.ncbi.nlm.nih.gov/pubmed/29150611 http://dx.doi.org/10.1038/s41467-017-01577-2 |
op_rights |
© The Author(s) 2017 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-017-01577-2 |
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Nature Communications |
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8 |
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1 |
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