Common Presence of 16O-rich Melilite in Calcium-Aluminum-rich Inclusions from the Least Metamorphosed CV Carbonaceous Chondrite Kaba

Details Common Presence of 16O-rich Melilite in Calcium-Aluminum-rich Inclusions from the Least Metamorphosed CV Carbonaceous Chondrite Kaba Common Presence of 16O-rich Melilite in Calcium-Aluminum-rich Inclusions from the Least Metamorphosed CV Carbonaceous Chondrite Kaba

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.2059n&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

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In contrast to commonly 16O-depleted melilite in CAIs from Allende
(CV>3.6), most melilite grains in Kaba (CV3.1) CAIs are 16O-rich,
suggesting a correlation between 16O-depletion in melilite of the CV
CAIs and petrologic type of a host meteorite.

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