Origin of the Refractory Component in Ferromagnesian Chondrules and Constraints on their Thermal Histories: Clues from Glass Inclusions in Olivine from Carbonaceous Chondrites
Abstract
Compositions of glass inclusions in olivine from CM, CR, and CV chondrites can be described as mixtures of Type C CAIs and SiO2 that are far from olivine saturation. This places severe constraints on possible thermal histories.
- Publication:
-
42nd Annual Lunar and Planetary Science Conference
- Pub Date:
- March 2011
- Bibcode:
- 2011LPI....42.2071B