Molecular and Isotopic Evolution of Insoluble Organic Matter of the Orgueil Meteorite upon Heating
Abstract
The Orgueil IOM was subjected to 300°C and 500°C under Ar flux to shed light on D-rich and 15N-rich organic components. The thermal evolution of H and N isotopes is decoupled, reflecting different behavior of these components hence different history.
- Publication:
-
82nd Annual Meeting of The Meteoritical Society
- Pub Date:
- July 2019
- Bibcode:
- 2019LPICo2157.6381R