Evidence for a serpentinized plate interface favouring continental subduction

The dynamics of continental subduction is largely controlled by the rheological properties of rocks involved along the subduction channel. Here, the authors reveal a prominent, yet previously undetected, low-velocity body beneath the Western Alps, along the plate interface between the European slab...

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Autores principales:	Liang Zhao, Marco G. Malusà, Huaiyu Yuan, Anne Paul, Stéphane Guillot, Yang Lu, Laurent Stehly, Stefano Solarino, Elena Eva, Gang Lu, Thomas Bodin, CIFALPS Group, AlpArray Working Group
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/7b8a2fed5f5e47e7a43d36077b7094e5
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spelling	oai:doaj.org-article:7b8a2fed5f5e47e7a43d36077b7094e52021-12-02T17:32:59ZEvidence for a serpentinized plate interface favouring continental subduction10.1038/s41467-020-15904-72041-1723https://doaj.org/article/7b8a2fed5f5e47e7a43d36077b7094e52020-05-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-15904-7https://doaj.org/toc/2041-1723The dynamics of continental subduction is largely controlled by the rheological properties of rocks involved along the subduction channel. Here, the authors reveal a prominent, yet previously undetected, low-velocity body beneath the Western Alps, along the plate interface between the European slab and the overlying Adriatic mantle, which they interpret as a serpentinite layer.Liang ZhaoMarco G. MalusàHuaiyu YuanAnne PaulStéphane GuillotYang LuLaurent StehlyStefano SolarinoElena EvaGang LuThomas BodinCIFALPS GroupAlpArray Working GroupNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Liang Zhao Marco G. Malusà Huaiyu Yuan Anne Paul Stéphane Guillot Yang Lu Laurent Stehly Stefano Solarino Elena Eva Gang Lu Thomas Bodin CIFALPS Group AlpArray Working Group Evidence for a serpentinized plate interface favouring continental subduction
description	The dynamics of continental subduction is largely controlled by the rheological properties of rocks involved along the subduction channel. Here, the authors reveal a prominent, yet previously undetected, low-velocity body beneath the Western Alps, along the plate interface between the European slab and the overlying Adriatic mantle, which they interpret as a serpentinite layer.
format	article
author	Liang Zhao Marco G. Malusà Huaiyu Yuan Anne Paul Stéphane Guillot Yang Lu Laurent Stehly Stefano Solarino Elena Eva Gang Lu Thomas Bodin CIFALPS Group AlpArray Working Group
author_facet	Liang Zhao Marco G. Malusà Huaiyu Yuan Anne Paul Stéphane Guillot Yang Lu Laurent Stehly Stefano Solarino Elena Eva Gang Lu Thomas Bodin CIFALPS Group AlpArray Working Group
author_sort	Liang Zhao
title	Evidence for a serpentinized plate interface favouring continental subduction
title_short	Evidence for a serpentinized plate interface favouring continental subduction
title_full	Evidence for a serpentinized plate interface favouring continental subduction
title_fullStr	Evidence for a serpentinized plate interface favouring continental subduction
title_full_unstemmed	Evidence for a serpentinized plate interface favouring continental subduction
title_sort	evidence for a serpentinized plate interface favouring continental subduction
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/7b8a2fed5f5e47e7a43d36077b7094e5
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Evidence for a serpentinized plate interface favouring continental subduction

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