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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Autores principales:	Ricarda Dziadek, Fausto Ferraccioli, Karsten Gohl
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Geology QE1-996.5 Environmental sciences GE1-350
Acceso en línea:	https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19
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id	oai:doaj.org-article:5f802c6d165b48c19608fe8c0f520c19
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spelling	oai:doaj.org-article:5f802c6d165b48c19608fe8c0f520c192021-12-02T16:45:45ZHigh geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data10.1038/s43247-021-00242-32662-4435https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c192021-08-01T00:00:00Zhttps://doi.org/10.1038/s43247-021-00242-3https://doaj.org/toc/2662-4435The 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.Ricarda DziadekFausto FerraccioliKarsten GohlNature PortfolioarticleGeologyQE1-996.5Environmental sciencesGE1-350ENCommunications Earth & Environment, Vol 2, Iss 1, Pp 1-6 (2021)
institution	DOAJ
collection	DOAJ
language	EN
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
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
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://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19
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High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data

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