Distribution of vanadium and melting of opaque assemblages in Efremovka CAI's

Details Distribution of vanadium and melting of opaque assemblages in Efremovka CAI's Distribution of vanadium and melting of opaque assemblages in Efremovka CAI's

Mar 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993lpi....24..257c&link_type=abstract

In Lunar and Planetary Inst., Twenty-fourth Lunar and Planetary Science Conference. Part 1: A-F p 257-258 (SEE N94-12015 01-91)

Computer Science

Carbonaceous Chondrites, Chemical Analysis, Inclusions, Meteoritic Composition, Petrography, Magnetite, Vanadium

Scientific paper

A 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.

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