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High Pressure Metamorphism Caused by Fluid Induced Weakening of Deep Continental Crust

Studies of mineral equilibria in metamorphic rocks have given valuable insights into the tectonic processes operating at convergent plate margins during an orogeny. Geodynamic models simulating orogenesis and crustal thickening have been constrained by temperature and pressure estimates inferred fro...

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Détails bibliographiques
Publié dans:Sci Rep
Auteurs principaux: Jamtveit, Bjørn, Moulas, Evangelos, Andersen, Torgeir B., Austrheim, Håkon, Corfu, Fernando, Petley-Ragan, Arianne, Schmalholz, Stefan M.
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group UK 2018
Sujets:
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC6242872/
https://ncbi.nlm.nih.gov/pubmed/30451887
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-35200-1
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