Buoyancy-driven, rapid exhumation of ultrahigh-pressure metamorphosed continental crust
Preservation of ultrahigh-pressure (UHP) minerals formed at depths of 90–125 km require unusual conditions. Our subduction model involves underflow of a salient (250 ± 150 km wide, 90–125 km long) of continental crust embedded in cold, largely oceanic crust-capped lithosphere; loss of leading portio...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
1997
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC23212/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11038569/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.94.18.9532 |
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