Contrasting Re/Os magmatic fractionation in planetary basalts

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Basalt, Chemical Fractionation, Lunar Rocks, Magma, Meteoritic Composition, Osmium Isotopes, Rhenium Isotopes, Achondrites, Chondrites, Geochemistry, Oxygen

Scientific paper

This work reports the first Re-Os isotopic results for lunar basalts and eucrites. Both Re and Os concentrations are found to be very low and Re/Os ratios are close to chondritic. This contrasts with the much higher than chondritic Re/Os ratio of terrestrial basalts. Osmium displays a rather uniform solid/liquid fractionation in different planetary bodies (Moon, Earth, Eucrite Parent Body, Mars), whereas rhenium is about three orders of magnitude more incompatible in terrestrial basalt genesis. We argue that this is a function of oxygen fugacity in the source regions of basalts.

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