Oceanic crust recycling controlled by weakening at slab edges

Retreating subduction zones are enabled by the development of faults at the edges of the slab, but the physical mechanisms controlling fault propagation remain debated. Here, the authors find that oceanic crust recycling is controlled by weakening of fractures forming at the edges of slabs.

Gespeichert in:

Autor*in:	Jessica Munch [verfasserIn] Taras Gerya [verfasserIn] Kosuke Ueda [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Übergeordnetes Werk:	In: Nature Communications - Nature Portfolio, 2016, 11(2020), 1, Seite 6
Übergeordnetes Werk:	volume:11 ; year:2020 ; number:1 ; pages:6

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1038/s41467-020-15750-7

Katalog-ID:	DOAJ004944674

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author	Jessica Munch
spellingShingle	Jessica Munch misc Science misc Q Oceanic crust recycling controlled by weakening at slab edges
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topic_title	Oceanic crust recycling controlled by weakening at slab edges
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title	Oceanic crust recycling controlled by weakening at slab edges
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title_sort	oceanic crust recycling controlled by weakening at slab edges
title_auth	Oceanic crust recycling controlled by weakening at slab edges
abstract	Retreating subduction zones are enabled by the development of faults at the edges of the slab, but the physical mechanisms controlling fault propagation remain debated. Here, the authors find that oceanic crust recycling is controlled by weakening of fractures forming at the edges of slabs.
abstractGer	Retreating subduction zones are enabled by the development of faults at the edges of the slab, but the physical mechanisms controlling fault propagation remain debated. Here, the authors find that oceanic crust recycling is controlled by weakening of fractures forming at the edges of slabs.
abstract_unstemmed	Retreating subduction zones are enabled by the development of faults at the edges of the slab, but the physical mechanisms controlling fault propagation remain debated. Here, the authors find that oceanic crust recycling is controlled by weakening of fractures forming at the edges of slabs.
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title_short	Oceanic crust recycling controlled by weakening at slab edges
url	https://doi.org/10.1038/s41467-020-15750-7 https://doaj.org/article/16fcad5ae9664232bb0d1f1d40cf0ae5 https://doaj.org/toc/2041-1723
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up_date	2024-07-04T01:45:40.508Z
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