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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 AugiteThe composition of the parent magma for the Nakhla (martian) meteorite has been estimated from mineral-melt partitioning and from magmatic inclusions in olivine and in augite. These independent lines of evidence have converged on small range of likely compositions. Additional information is contained in the original extended abstract.
Document ID
20010044721
Document Type
Conference Paper
Authors
Treiman, Allan H. (Lunar and Planetary Inst. Houston, TX United States)
Goodrich, Cyrena Anne (Max-Planck-Inst. fuer Chemie Mainz, Germany)
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Publication Information
Publication: Lunar and Planetary Science XXXII
Subject Category
Lunar And Planetary Science And Exploration
Funding Number(s)
CONTRACT_GRANT: NAG5-8270
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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