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...

Full description

Saved in:

Bibliographic Details
Main Authors:	Armel Menant, Samuel Angiboust, Taras Gerya, Robin Lacassin, Martine Simoes, Raphael Grandin
Format:	article
Language:	EN
Published:	Nature Portfolio 2020
Subjects:	Science Q
Online Access:	https://doaj.org/article/947c31e42d2a44c6a28fd5baf0c9c63d
Tags:	Add Tag No Tags, Be the first to tag this record!

id	oai:doaj.org-article:947c31e42d2a44c6a28fd5baf0c9c63d
record_format	dspace
spelling	oai:doaj.org-article:947c31e42d2a44c6a28fd5baf0c9c63d2021-12-02T14:41:26ZTransient stripping of subducting slabs controls periodic forearc uplift10.1038/s41467-020-15580-72041-1723https://doaj.org/article/947c31e42d2a44c6a28fd5baf0c9c63d2020-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-15580-7https://doaj.org/toc/2041-1723Topography 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.Armel MenantSamuel AngiboustTaras GeryaRobin LacassinMartine SimoesRaphael GrandinNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Armel Menant Samuel Angiboust Taras Gerya Robin Lacassin Martine Simoes Raphael Grandin Transient stripping of subducting slabs controls periodic forearc uplift
description	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.
format	article
author	Armel Menant Samuel Angiboust Taras Gerya Robin Lacassin Martine Simoes Raphael Grandin
author_facet	Armel Menant Samuel Angiboust Taras Gerya Robin Lacassin Martine Simoes Raphael Grandin
author_sort	Armel Menant
title	Transient stripping of subducting slabs controls periodic forearc uplift
title_short	Transient stripping of subducting slabs controls periodic forearc uplift
title_full	Transient stripping of subducting slabs controls periodic forearc uplift
title_fullStr	Transient stripping of subducting slabs controls periodic forearc uplift
title_full_unstemmed	Transient stripping of subducting slabs controls periodic forearc uplift
title_sort	transient stripping of subducting slabs controls periodic forearc uplift
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/947c31e42d2a44c6a28fd5baf0c9c63d
work_keys_str_mv	AT armelmenant transientstrippingofsubductingslabscontrolsperiodicforearcuplift AT samuelangiboust transientstrippingofsubductingslabscontrolsperiodicforearcuplift AT tarasgerya transientstrippingofsubductingslabscontrolsperiodicforearcuplift AT robinlacassin transientstrippingofsubductingslabscontrolsperiodicforearcuplift AT martinesimoes transientstrippingofsubductingslabscontrolsperiodicforearcuplift AT raphaelgrandin transientstrippingofsubductingslabscontrolsperiodicforearcuplift
_version_	1718389884038676480

Transient stripping of subducting slabs controls periodic forearc uplift

Similar Items