A new method to quantitatively control oxygen fugacity in externally heated pressure vessel experiments
<p>Oxygen fugacity (<span class="inline-formula"><i>f</i>O<sub>2</sub></span>) is a fundamental variable affecting phase equilibrium in magmas, and in externally heated pressure vessel experiments it is typically controlled by using redox buffer as...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-02-01
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| Series: | European Journal of Mineralogy |
| Online Access: | https://ejm.copernicus.org/articles/32/219/2020/ejm-32-219-2020.pdf |