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...
Enregistré dans:
Auteurs principaux: | Armel Menant, Samuel Angiboust, Taras Gerya, Robin Lacassin, Martine Simoes, Raphael Grandin |
---|---|
Format: | article |
Langue: | EN |
Publié: |
Nature Portfolio
2020
|
Sujets: | |
Accès en ligne: | https://doaj.org/article/947c31e42d2a44c6a28fd5baf0c9c63d |
Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
Documents similaires
-
Pervasive subduction zone devolatilization recycles CO2 into the forearc
par: E. M. Stewart, et autres
Publié: (2020) -
Oceanic crust recycling controlled by weakening at slab edges
par: Jessica Munch, et autres
Publié: (2020) -
No significant boron in the hydrated mantle of most subducting slabs
par: Andrew M. McCaig, et autres
Publié: (2018) -
Tracing the subducting Pacific slab to the mantle transition zone with hydrogen isotopes
par: Takeshi Kuritani, et autres
Publié: (2021) -
Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
par: Cheng Xu, et autres
Publié: (2018)