Fluid-rock interaction processes in ancient subduction zones evidenced by the high-pressure–low-temperature Acatlán complex, Mexico
Abstract Subduction zones play a crucial role in controlling interactions between the oceanic crust and mantle, generating fluid and hydrous melt, and facilitating subsequent volatile and mass transfer to mantle depths. In the Acatlán Complex, Mexico, trace elements, Sr–Nd isotopes, petrological mod...
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| Asıl Yazarlar: | , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2025-04-01
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| Seri Bilgileri: | Scientific Reports |
| Konular: | |
| Online Erişim: | https://doi.org/10.1038/s41598-025-93279-9 |
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