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Reaction-induced rheological weakening enables oceanic plate subduction

Earth is the only terrestrial planet in our solar system where an oceanic plate subducts beneath an overriding plate. Although the initiation of plate subduction requires extremely weak boundaries between strong plates, the way in which oceanic mantle rheologically weakens remains unknown. Here we s...

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Détails bibliographiques
Publié dans:Nat Commun
Auteurs principaux: Hirauchi, Ken-ichi, Fukushima, Kumi, Kido, Masanori, Muto, Jun, Okamoto, Atsushi
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group 2016
Sujets:
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC5007449/
https://ncbi.nlm.nih.gov/pubmed/27562366
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms12550
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