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The Garnet to Majorite Transformation in Mafic CompositionsThe garnet to majorite transformation in mafic compositions is controlled by bulk composition and the presence of silicate melt, clinopyroxene, and silicate perovskite as well as pressure. Thus, the use of empirical geobarometers based on garnet Si(4+) and/or [Al(3+) +/- Cr(3+)] (p.f.u) seems unjustified. Additional information is contained in the original extended abstract.
Document ID
20020045852
Acquisition Source
Johnson Space Center
Document Type
Conference Paper
Authors
Xirouchakis, D. (NASA Johnson Space Center Houston, TX United States)
Draper, David S. (NASA Johnson Space Center Houston, TX United States)
Agee, C. B. (NASA Johnson Space Center Houston, TX United States)
Date Acquired
August 20, 2013
Publication Date
April 1, 2002
Publication Information
Publication: Lunar and Planetary Science XXXIII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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