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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Autor*in:	Liang Zhao [verfasserIn] Marco G. Malusà [verfasserIn] Huaiyu Yuan [verfasserIn] Anne Paul [verfasserIn] Stéphane Guillot [verfasserIn] Yang Lu [verfasserIn] Laurent Stehly [verfasserIn] Stefano Solarino [verfasserIn] Elena Eva [verfasserIn] Gang Lu [verfasserIn] Thomas Bodin [verfasserIn] CIFALPS Group [verfasserIn] AlpArray Working Group [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Übergeordnetes Werk:	In: Nature Communications - Nature Portfolio, 2016, 11(2020), 1, Seite 8
Übergeordnetes Werk:	volume:11 ; year:2020 ; number:1 ; pages:8

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1038/s41467-020-15904-7

Katalog-ID:	DOAJ051200678

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author	Liang Zhao
spellingShingle	Liang Zhao misc Science misc Q Evidence for a serpentinized plate interface favouring continental subduction
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topic_title	Evidence for a serpentinized plate interface favouring continental subduction
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title	Evidence for a serpentinized plate interface favouring continental subduction
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title_full	Evidence for a serpentinized plate interface favouring continental subduction
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author_browse	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
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title_sort	evidence for a serpentinized plate interface favouring continental subduction
title_auth	Evidence for a serpentinized plate interface favouring continental subduction
abstract	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.
abstractGer	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.
abstract_unstemmed	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.
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title_short	Evidence for a serpentinized plate interface favouring continental subduction
url	https://doi.org/10.1038/s41467-020-15904-7 https://doaj.org/article/7b8a2fed5f5e47e7a43d36077b7094e5 https://doaj.org/toc/2041-1723
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score	7.4019346

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Evidence for a serpentinized plate interface favouring continental subduction

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