Oxygen Isotopic Compositions of Fayalite in the CV Chondrite Kaba
Abstract
The oxygen isotopic compositions of fayalite grains in the CV3 carbonaceous chondrites Kaba bring information on the origin of water accreted by the CV parent body and its isotopic evolution during secondary alteration processes.
- Publication:
-
80th Annual Meeting of the Meteoritical Society
- Pub Date:
- July 2017
- Bibcode:
- 2017LPICo1987.6179M