Transient stripping of subducting slabs controls periodic forearc uplift

Topography at active forearc margins is controlled by numerous competing tectonic and erosional processes acting at different timescales, yet separating their respective contribution remains a challenge. Here, the authors evidence Myr-scale, uplift-then-subsidence cycles controlled by transient accr...
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Autor*in:	Armel Menant [verfasserIn] Samuel Angiboust [verfasserIn] Taras Gerya [verfasserIn] Robin Lacassin [verfasserIn] Martine Simoes [verfasserIn] Raphael Grandin [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Übergeordnetes Werk:	In: Nature Communications - Nature Portfolio, 2016, 11(2020), 1, Seite 10
Übergeordnetes Werk:	volume:11 ; year:2020 ; number:1 ; pages:10

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1038/s41467-020-15580-7

Katalog-ID:	DOAJ052746232

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author	Armel Menant
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topic_title	Transient stripping of subducting slabs controls periodic forearc uplift
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title	Transient stripping of subducting slabs controls periodic forearc uplift
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title_full	Transient stripping of subducting slabs controls periodic forearc uplift
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title_sort	transient stripping of subducting slabs controls periodic forearc uplift
title_auth	Transient stripping of subducting slabs controls periodic forearc uplift
abstract	Topography at active forearc margins is controlled by numerous competing tectonic and erosional processes acting at different timescales, yet separating their respective contribution remains a challenge. Here, the authors evidence Myr-scale, uplift-then-subsidence cycles controlled by transient accretion at the base of the forearc domain.
abstractGer	Topography at active forearc margins is controlled by numerous competing tectonic and erosional processes acting at different timescales, yet separating their respective contribution remains a challenge. Here, the authors evidence Myr-scale, uplift-then-subsidence cycles controlled by transient accretion at the base of the forearc domain.
abstract_unstemmed	Topography at active forearc margins is controlled by numerous competing tectonic and erosional processes acting at different timescales, yet separating their respective contribution remains a challenge. Here, the authors evidence Myr-scale, uplift-then-subsidence cycles controlled by transient accretion at the base of the forearc domain.
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title_short	Transient stripping of subducting slabs controls periodic forearc uplift
url	https://doi.org/10.1038/s41467-020-15580-7 https://doaj.org/article/947c31e42d2a44c6a28fd5baf0c9c63d https://doaj.org/toc/2041-1723
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