Fe2+–Mg partitioning between olivine and basaltic melts: Applications to genesis of olivine-phyric shergottites and conditions of melting in the Martian interior
- 15 April 2011
- journal article
- research article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 304 (3-4), 527-537
- https://doi.org/10.1016/j.epsl.2011.02.029
Abstract
No abstract availableKeywords
Funding Information
- National Aeronautics and Space Administration (NNX09AL25G)
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