Formation of the Xigaze Metamorphic Sole under Tibetan continental lithosphere reveals generic characteristics of subduction initiation
Abstract Metamorphic soles found under allochthonous oceanic lithosphere, or ophiolites, are interpreted as derived from lower plate oceanic crust material accreted to upper plate mantle during intraoceanic subduction initiation. Their metamorphic evolution is inferred to reflect the thermal structu...
| Hlavní autoři: | , , , , , , , , |
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| Médium: | Článek |
| Jazyk: | English |
| Vydáno: |
Nature Portfolio
2023-09-01
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| Edice: | Communications Earth & Environment |
| On-line přístup: | https://doi.org/10.1038/s43247-023-01007-w |