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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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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acesso em linha: | 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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