Formation of P-Rich Olivine in DaG 978 Carbonaceous Chondrite Through Fluid-Assisted Metamorphism
Abstract
We describe an occurrence of P-rich olivine in the DaG 978 carbonaceous chondrite. Different from other natural P-rich olivine, the P-rich olivine should have formed through fluid-assisted metamorphism.
- Publication:
-
79th Annual Meeting of the Meteoritical Society
- Pub Date:
- August 2016
- Bibcode:
- 2016LPICo1921.6002Z