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Water transport to the core–mantle boundary
Water is transported to Earth's interior in lithospheric slabs at subduction zones. Shallow dehydration fuels hydrous island arc magmatism but some water is transported deeper in cool slab mantle. Further dehydration at ∼700 km may limit deeper transport but hydrated phases in slab crust have c...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Oxford University Press
2021
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288335/ https://www.ncbi.nlm.nih.gov/pubmed/34691622 http://dx.doi.org/10.1093/nsr/nwab007 |
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author | Walter, Michael J |
author_facet | Walter, Michael J |
author_sort | Walter, Michael J |
collection | PubMed |
description | Water is transported to Earth's interior in lithospheric slabs at subduction zones. Shallow dehydration fuels hydrous island arc magmatism but some water is transported deeper in cool slab mantle. Further dehydration at ∼700 km may limit deeper transport but hydrated phases in slab crust have considerable capacity for transporting water to the core-mantle boundary. Quantifying how much remains the challenge. |
format | Online Article Text |
id | pubmed-8288335 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | Oxford University Press |
record_format | MEDLINE/PubMed |
spelling | pubmed-82883352021-10-21 Water transport to the core–mantle boundary Walter, Michael J Natl Sci Rev EARTH SCIENCES Water is transported to Earth's interior in lithospheric slabs at subduction zones. Shallow dehydration fuels hydrous island arc magmatism but some water is transported deeper in cool slab mantle. Further dehydration at ∼700 km may limit deeper transport but hydrated phases in slab crust have considerable capacity for transporting water to the core-mantle boundary. Quantifying how much remains the challenge. Oxford University Press 2021-01-12 /pmc/articles/PMC8288335/ /pubmed/34691622 http://dx.doi.org/10.1093/nsr/nwab007 Text en © The Author(s) 2021. Published by Oxford University Press on behalf of China Science Publishing & Media Ltd. https://creativecommons.org/licenses/by/4.0/This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) ), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. |
spellingShingle | EARTH SCIENCES Walter, Michael J Water transport to the core–mantle boundary |
title | Water transport to the core–mantle boundary |
title_full | Water transport to the core–mantle boundary |
title_fullStr | Water transport to the core–mantle boundary |
title_full_unstemmed | Water transport to the core–mantle boundary |
title_short | Water transport to the core–mantle boundary |
title_sort | water transport to the core–mantle boundary |
topic | EARTH SCIENCES |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288335/ https://www.ncbi.nlm.nih.gov/pubmed/34691622 http://dx.doi.org/10.1093/nsr/nwab007 |
work_keys_str_mv | AT waltermichaelj watertransporttothecoremantleboundary |