Oxygen Isotopic Compositions of Fayalite in the Kaba Cv3 Carbonaceous Chondrite
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چکیده
INTRODUCTION The Fe-rich olivine end-member, fayalite (Fa100), occurs in the matrix, chondrules, CAIs, silicate aggregates, and dark inclusions in the oxidized Kaba and Mokoia CV3 chondrites, where it is associated with magnetite and troilite. To help constrain the origin of the fayalite, we measured O-isotope compositions of fayalite (Fa98-100) from two petrographic settings of the Kaba meteorite using the ion probe at ASU.
منابع مشابه
Fayalite in the Vigarano CV3 carbonaceous chondrite: Occurrences, formation age and conditions
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تاریخ انتشار 2003