Accretion and Disruption Histories of the Ordinary Chondrite Parent Bodies
Abstract
Discrepant Pb-Pb phosphate ages and Ni-metal metallographic cooling rates for ordinary chondrites may be explained by a decoupling of the two systems along parent body cooling paths interrupted by a catastrophic disruption at 60 My after CAIs.
- Publication:
-
80th Annual Meeting of the Meteoritical Society
- Pub Date:
- July 2017
- Bibcode:
- 2017LPICo1987.6367E