Correlations Between Surficial Sulfur and a Crustal Assimilation Signature in Martian Shergottites
Abstract
The La/Sm ratios of shergottites reflect the degree to which they have assimilated martian crust. Shergottites with low La/Sm ratios show small or no ∆S-33 anomalies. Those shergottites with large positive ∆S-33 anomalies also have higher La/Sm ratios.
- Publication:
-
77th Annual Meeting of the Meteoritical Society
- Pub Date:
- September 2014
- Bibcode:
- 2014LPICo1800.5076J