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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Detalles Bibliográficos
Autores principales: Jamtveit, Bjørn, Moulas, Evangelos, Andersen, Torgeir B., Austrheim, Håkon, Corfu, Fernando, Petley-Ragan, Arianne, Schmalholz, Stefan M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6242872/
https://www.ncbi.nlm.nih.gov/pubmed/30451887
http://dx.doi.org/10.1038/s41598-018-35200-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6242872/
https://www.ncbi.nlm.nih.gov/pubmed/30451887
http://dx.doi.org/10.1038/s41598-018-35200-1

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