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.

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Ricarda Dziadek, Fausto Ferraccioli, Karsten Gohl
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2021
Subjects:
geo
envir
Amundsen Sea
Antarctic
Thwaites Glacier
West Antarctica
Antarc*
Antarctica
Online Access:https://doi.org/10.1038/s43247-021-00242-3
https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19
id fttriple:oai:gotriple.eu:oai:doaj.org/article:5f802c6d165b48c19608fe8c0f520c19
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spelling fttriple:oai:gotriple.eu: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 2021-08-01 https://doi.org/10.1038/s43247-021-00242-3 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 en eng Nature Portfolio doi:10.1038/s43247-021-00242-3 2662-4435 https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19 undefined Communications Earth & Environment, Vol 2, Iss 1, Pp 1-6 (2021) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2021 fttriple https://doi.org/10.1038/s43247-021-00242-3 2023-01-22T18:11:39Z 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 Unknown Amundsen Sea Antarctic Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) West Antarctica Communications Earth & Environment 2 1
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
Ricarda Dziadek
Fausto Ferraccioli
Karsten Gohl
High geothermal heat flow beneath Thwaites Glacier in West Antarctica inferred from aeromagnetic data
topic_facet geo
envir
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 Amundsen Sea
Antarctic
Thwaites Glacier
West Antarctica
geographic_facet Amundsen Sea
Antarctic
Thwaites Glacier
West Antarctica
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 doi:10.1038/s43247-021-00242-3
2662-4435
https://doaj.org/article/5f802c6d165b48c19608fe8c0f520c19
op_rights undefined
op_doi https://doi.org/10.1038/s43247-021-00242-3
container_title Communications Earth & Environment
container_volume 2
container_issue 1
_version_ 1766374028765822976

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