The compatibility of rhenium and osmium in natural olivine and their behaviour during mantle melting and basalt genesis
Rhenium and osmium (Re-Os) elemental abundances have been obtained for magmatic olivine from a range of host basalt compositions, for mantle olivine and coexisting phases (silicate and sulphide) from a spinel-peridotite, and olivine and Fe-Ni metal from Pallasite meteorites. These data indicate that...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Journal article |
| Language: | English |
| Published: |
2002
|