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Evidence for ultramafic lavas on Syrtis MajorPyroxene compositions from ISM data compared with pyroxene compositions of Apollo 12 pigeonite basalt, Shergotite meteorite, and pyroxenitic komatiite show that the Syrtis Major volcanic materials are consistent with pyroxenitic komatiite. Pyroxenitic komatiite is significant for the earth because it contains a large amount of MgO, implying generation under unique circumstances compared to typical basaltic compositions.
Document ID
19940028723
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Reyes, D. P.
(Arizona State Univ. Tempe, AZ, United States)
Christensen, P. R.
(Arizona State Univ. Tempe, AZ, United States)
Date Acquired
September 6, 2013
Publication Date
January 1, 1993
Publication Information
Publication: Lunar and Planetary Inst., Mars: Past, Present, and Future. Results from the MSATT Program, Part 1
Subject Category
Lunar And Planetary Exploration
Accession Number
94N33229
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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