Effect of oxygen fugacity on the storage of water in wadsleyite and olivine in H and H–C fluids and implications for melting atop the transition zone
<p>This study aims to experimentally constrain the water storage capacities of olivine and wadsleyite at a depth near 410 km (12–14 GPa) under water-saturated conditions, as a function of temperature, oxygen fugacity, and the presence of carbon (molar H <span class="inline-formula"...
| Hlavní autoři: | , , , , |
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| Médium: | Článek |
| Jazyk: | English |
| Vydáno: |
Copernicus Publications
2023-07-01
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| Edice: | European Journal of Mineralogy |
| On-line přístup: | https://ejm.copernicus.org/articles/35/549/2023/ejm-35-549-2023.pdf |