Chargement en cours...
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...
Enregistré dans:
| Publié dans: | Sci Rep |
|---|---|
| Auteurs principaux: | , , , , , , |
| 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 |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|