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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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| 主要な著者: | , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
The National Academy of Sciences of the USA
1997
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC23212/ https://ncbi.nlm.nih.gov/pubmed/11038569 |
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