Forsterite-rich Accretionary Rims Around CAIs from the Reduced CV3 Chondrite Efremovka: I. Mineralogy and Petrography

Details Forsterite-rich Accretionary Rims Around CAIs from the Reduced CV3 Chondrite Efremovka: I. Mineralogy and Petrography Forsterite-rich Accretionary Rims Around CAIs from the Reduced CV3 Chondrite Efremovka: I. Mineralogy and Petrography

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1239k&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1239

Computer Science

Scientific paper

Accretionary rims around Type A and B CAIs from the reduced CV3
chondrite Efremovka are aggregates of high-temperature nebular
condensates composed of forsterite, Fe,Ni-metal and a refractory
component composed of Al-diopside, anorthite, and spinel.

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