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Slab melting versus slab dehydration in subduction-zone magmatism
The second critical endpoint in the basalt-H(2)O system was directly determined by a high-pressure and high-temperature X-ray radiography technique. We found that the second critical endpoint occurs at around 3.4 GPa and 770 °C (corresponding to a depth of approximately 100 km in a subducting slab),...
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| Main Authors: | , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2011
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3100975/ https://ncbi.nlm.nih.gov/pubmed/21536910 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1010968108 |
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