Microscale Distribution and Behavior of Th and K in Late-Stage Melts and Shock Melts in Olivine-Phyric Shergottites: Implications for the Interpretation of Remote Sensing and In Situ Measurements of the Martian Surface

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Scientific paper

Th and K in many of the Mars surface lithologies are not reflected in
the martian meteorite collection. In this study, we examine the
variation in Sm, Th, K, and major elements in both late stage-melt and
shock-melt assemblages in martian meteorites.

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