Dehydration-driven stress transfer triggers intermediate-depth earthquakes

Intermediate-depth earthquakes (30-300 km) occur in subducting oceanic slabs, but their generation mechanism remains enigmatic. Here, the authors show through high-pressure and dehydration experiments of antigorite that dehydration-driven stress transfer triggers intermediate-depth earthquakes.

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Autores principales: Thomas P. Ferrand, Nadège Hilairet, Sarah Incel, Damien Deldicque, Loïc Labrousse, Julien Gasc, Joerg Renner, Yanbin Wang, Harry W. Green II, Alexandre Schubnel
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/49e8bc4237ca4c9e8c6a7ef1adb47523
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spelling oai:doaj.org-article:49e8bc4237ca4c9e8c6a7ef1adb475232021-12-02T14:41:18ZDehydration-driven stress transfer triggers intermediate-depth earthquakes10.1038/ncomms152472041-1723https://doaj.org/article/49e8bc4237ca4c9e8c6a7ef1adb475232017-05-01T00:00:00Zhttps://doi.org/10.1038/ncomms15247https://doaj.org/toc/2041-1723Intermediate-depth earthquakes (30-300 km) occur in subducting oceanic slabs, but their generation mechanism remains enigmatic. Here, the authors show through high-pressure and dehydration experiments of antigorite that dehydration-driven stress transfer triggers intermediate-depth earthquakes.Thomas P. FerrandNadège HilairetSarah IncelDamien DeldicqueLoïc LabrousseJulien GascJoerg RennerYanbin WangHarry W. Green IIAlexandre SchubnelNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-11 (2017)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Thomas P. Ferrand
Nadège Hilairet
Sarah Incel
Damien Deldicque
Loïc Labrousse
Julien Gasc
Joerg Renner
Yanbin Wang
Harry W. Green II
Alexandre Schubnel
Dehydration-driven stress transfer triggers intermediate-depth earthquakes
description Intermediate-depth earthquakes (30-300 km) occur in subducting oceanic slabs, but their generation mechanism remains enigmatic. Here, the authors show through high-pressure and dehydration experiments of antigorite that dehydration-driven stress transfer triggers intermediate-depth earthquakes.
format article
author Thomas P. Ferrand
Nadège Hilairet
Sarah Incel
Damien Deldicque
Loïc Labrousse
Julien Gasc
Joerg Renner
Yanbin Wang
Harry W. Green II
Alexandre Schubnel
author_facet Thomas P. Ferrand
Nadège Hilairet
Sarah Incel
Damien Deldicque
Loïc Labrousse
Julien Gasc
Joerg Renner
Yanbin Wang
Harry W. Green II
Alexandre Schubnel
author_sort Thomas P. Ferrand
title Dehydration-driven stress transfer triggers intermediate-depth earthquakes
title_short Dehydration-driven stress transfer triggers intermediate-depth earthquakes
title_full Dehydration-driven stress transfer triggers intermediate-depth earthquakes
title_fullStr Dehydration-driven stress transfer triggers intermediate-depth earthquakes
title_full_unstemmed Dehydration-driven stress transfer triggers intermediate-depth earthquakes
title_sort dehydration-driven stress transfer triggers intermediate-depth earthquakes
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/49e8bc4237ca4c9e8c6a7ef1adb47523
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