The effect of oxygen fugacity on the partitioning of Re between crystals and silicate melt during mantle melting
Interpretation of Re-Os isotopic systematics applied to mantle and mantle-derived rocks is currently hindered by the poorly understood behaviour of Re and Os during partial melting. Of particular interest is the incompatibility of Re and how it partitions between melt and the different mantle phases. Here, we study the partitioning behaviour of Re between the common upper mantle minerals (garnet, spinel, clinopyroxene, orthopyroxene, and olivine) and silicate melt under temperature (1275-1450...[Show more]
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|Source:||Geochimica et Cosmochimica Acta|
|01_Mallmann_The_effect_of_oxygen_fugacity_2007.pdf||581.36 kB||Adobe PDF||Request a copy|
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