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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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Detalhes bibliográficos
Main Authors: Mibe, Kenji, Kawamoto, Tatsuhiko, Matsukage, Kyoko N., Fei, Yingwei, Ono, Shigeaki
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2011
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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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