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Arc magmas oxidised by water dissociation and hydrogen incorporation in orthopyroxene
Elevated H(2)O concentrations and oxygen fugacities are two fundamental properties that distinguish magmas formed in subduction zones from new crust generated at mid ocean ridges. However, the mechanism of magma oxidation, and how it relates to the increase in H(2)O remains unclear. In this study, w...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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2019
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6675610/ https://www.ncbi.nlm.nih.gov/pubmed/31372181 http://dx.doi.org/10.1038/s41561-019-0411-x |