Origin of Spinel Framboids in Calcium-Aluminum-Rich Inclusions
Abstract
Mineralogical, petrological and O-isotopic study of a CV CAI suggests that spinel framboids in the CAI were originally mini-CAIs that condensed separately under different conditions and subsequently aggregated to form the inclusion.
- Publication:
-
80th Annual Meeting of the Meteoritical Society
- Pub Date:
- July 2017
- Bibcode:
- 2017LPICo1987.6020Y