Transient stripping of subducting slabs controls periodic forearc uplift

Topography in forearc regions reflects tectonic processes along the subduction interface, from seismic cycle-related transients to long-term competition between accretion and erosion. Yet, no consensus exists about the topography drivers, especially as the contribution of deep accretion remains poor...

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Detalles Bibliográficos
Autores principales: Menant, Armel, Angiboust, Samuel, Gerya, Taras, Lacassin, Robin, Simoes, Martine, Grandin, Raphael
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7156703/
https://www.ncbi.nlm.nih.gov/pubmed/32286304
http://dx.doi.org/10.1038/s41467-020-15580-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7156703/
https://www.ncbi.nlm.nih.gov/pubmed/32286304
http://dx.doi.org/10.1038/s41467-020-15580-7

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