High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data
The Amundsen Sea sector, Antarctica, is underlain by shallow Curie depths – where the magnetic properties of rocks change – according to airborne magnetic data. This suggests high geothermal heat flow in this region of the West Antarctic Rift System.
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2021
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Online Access: | https://doi.org/10.1038/s43247-021-00242-3 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 |
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ftdoajarticles:oai:doaj.org/article:5f802c6d165b48c19608fe8c0f520c19 2023-05-15T13:23:41+02:00 High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data Ricarda Dziadek Fausto Ferraccioli Karsten Gohl 2021-08-01T00:00:00Z https://doi.org/10.1038/s43247-021-00242-3 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 EN eng Nature Portfolio https://doi.org/10.1038/s43247-021-00242-3 https://doaj.org/toc/2662-4435 doi:10.1038/s43247-021-00242-3 2662-4435 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 Communications Earth & Environment, Vol 2, Iss 1, Pp 1-6 (2021) Geology QE1-996.5 Environmental sciences GE1-350 article 2021 ftdoajarticles https://doi.org/10.1038/s43247-021-00242-3 2022-12-31T11:19:04Z The Amundsen Sea sector, Antarctica, is underlain by shallow Curie depths – where the magnetic properties of rocks change – according to airborne magnetic data. This suggests high geothermal heat flow in this region of the West Antarctic Rift System. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctica Thwaites Glacier West Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic West Antarctica Amundsen Sea Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) Communications Earth & Environment 2 1 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Geology QE1-996.5 Environmental sciences GE1-350 |
spellingShingle |
Geology QE1-996.5 Environmental sciences GE1-350 Ricarda Dziadek Fausto Ferraccioli Karsten Gohl High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data |
topic_facet |
Geology QE1-996.5 Environmental sciences GE1-350 |
description |
The Amundsen Sea sector, Antarctica, is underlain by shallow Curie depths – where the magnetic properties of rocks change – according to airborne magnetic data. This suggests high geothermal heat flow in this region of the West Antarctic Rift System. |
format |
Article in Journal/Newspaper |
author |
Ricarda Dziadek Fausto Ferraccioli Karsten Gohl |
author_facet |
Ricarda Dziadek Fausto Ferraccioli Karsten Gohl |
author_sort |
Ricarda Dziadek |
title |
High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data |
title_short |
High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data |
title_full |
High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data |
title_fullStr |
High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data |
title_full_unstemmed |
High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data |
title_sort |
high geothermal heat flow beneath thwaites glacier in west antarctica inferred from aeromagnetic data |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doi.org/10.1038/s43247-021-00242-3 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 |
long_lat |
ENVELOPE(-106.750,-106.750,-75.500,-75.500) |
geographic |
Antarctic West Antarctica Amundsen Sea Thwaites Glacier |
geographic_facet |
Antarctic West Antarctica Amundsen Sea Thwaites Glacier |
genre |
Amundsen Sea Antarc* Antarctic Antarctica Thwaites Glacier West Antarctica |
genre_facet |
Amundsen Sea Antarc* Antarctic Antarctica Thwaites Glacier West Antarctica |
op_source |
Communications Earth & Environment, Vol 2, Iss 1, Pp 1-6 (2021) |
op_relation |
https://doi.org/10.1038/s43247-021-00242-3 https://doaj.org/toc/2662-4435 doi:10.1038/s43247-021-00242-3 2662-4435 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 |
op_doi |
https://doi.org/10.1038/s43247-021-00242-3 |
container_title |
Communications Earth & Environment |
container_volume |
2 |
container_issue |
1 |
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1766374179449339904 |