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A parent magma for the Nakhla Martian meteorite: Reconciliation of estimates from 1-bar experiments, magmatic inclusions in olivine, and magmatic inclusions in augite

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Goodrich,  C. A.
Cosmochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Treiman, A. H., & Goodrich, C. A. (2001). A parent magma for the Nakhla Martian meteorite: Reconciliation of estimates from 1-bar experiments, magmatic inclusions in olivine, and magmatic inclusions in augite. In Lunar and Planetary Science XXXII. Houston: Lunar and Planetary Institute.


引用: https://hdl.handle.net/11858/00-001M-0000-0014-9266-3
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