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Distribution of vanadium and melting of opaque assemblages in Efremovka CAI'sA petrographic and chemical study of compact Type A CAI's from the Efremovka CV3 chondrite strongly suggests that the opaque assemblages (OA's) that they contain were molten at temperatures below the CAI silicate solidus, and that the V-rich magnetite presently observed in association with OA's formed by in situ oxidation of their FeNi.
Document ID
19940007669
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Casanova, I. (Field Museum of Natural History Chicago, IL, United States)
Grossman, L. (Chicago Univ. IL., United States)
Date Acquired
September 6, 2013
Publication Date
January 1, 1993
Publication Information
Publication: Lunar and Planetary Inst., Twenty-fourth Lunar and Planetary Science Conference. Part 1: A-F
Subject Category
Geophysics
Accession Number
94N12141
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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IDRelationTitle19940007055Collected WorksSixth Annual Workshop on Space Operations Applications and Research (SOAR 1992), volume 219940007543Collected WorksTwenty-fourth Lunar and Planetary Science Conference. Part 1: A-F
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