A geochemical study of the winonaites: Evidence for limited partial melting and constraints on the precursor composition
The winonaites are primitive achondrites which are associated with the IAB iron meteorites. Textural evidence implies heating to at least the Fe, Ni–FeS cotectic, but previous geochemical studies are ambiguous about the extent of silicate melting in these samples. Oxygen isotope evidence indicates t...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Pergamon
2017
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| Online Access: | http://hdl.handle.net/20.500.11937/29785 |