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Published in 2020 at "European Journal of Mineralogy"
DOI: 10.5194/ejm-32-219-2020
Abstract: Abstract. Oxygen fugacity (fO2) is a fundamental variable affecting phase equilibrium in magmas, and in externally heated pressure vessel experiments it is typically controlled by using redox buffer assemblages. However, these do not allow fine…
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Keywords:
pressure vessel;
heated pressure;
oxygen fugacity;
externally heated ... See more keywords