Original paper
The behaviour of ferric iron during partial melting of peridotite
Abstract
In order to better understand the behaviour of Fe3+ during partial melting of a mid-ocean-ridge-basalt (MORB) mantle source, we performed partial melting experiments of a spinel peridotite at 1.5 GPa, between 1320 and 1450 °C, and over a range of oxygen fugacities (fO2) varying from FMQ-3.5 to FMQ+6 (log-units relative to FMQ = Fayalite-Magnetite-Quartz oxygen buffer). Changes in fO2 were achieved using different capsule materials and by varying...
Paper Details
Title
The behaviour of ferric iron during partial melting of peridotite
Published Date
Oct 1, 2018
Volume
239
Pages
235 - 254
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History