Fast Cooling History of the Chassigny Martian Meteorite
Abstract
Pyroxene exsolution feature and chemical zoning of olivine in Chassigny suggest fast cooling history of this dunite meteorite. The final solidification of Chassigny seems to have occurred near the surface of the Mars.
- Publication:
-
Lunar and Planetary Science Conference
- Pub Date:
- March 2004
- Bibcode:
- 2004LPI....35.1535M