Geochemical modeling for martian enriched reservoir

Abstract

The magma evolution processes at shallow level in Mars are still obscure. Shergotty meteorite is a basaltic shergottite that is considered to be contaminated by enriched material. Y9810459, on the other hand, is considered to be a primitive magma among the basaltic shergottites. In this study, we will provide a new model about the enriched reservoir in Mars.