Replication Data for: Chalcophile elements in Martian meteorites indicate low sulfur content in the Martian interior and a volatile element-depleted late veneer.
收藏DataCite Commons2023-04-14 更新2025-04-15 收录
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https://planetary-data-portal.org/citation?persistentId=doi:10.35003/BMFSHW
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资源简介：
• Ratios of Cu, S, Se, Te, Re, Pt and Pd in Martian meteorites are relatively constant. • Martian meteorites show very limited eruptive losses of volatile Re, S, Se and Te. • The parent magmas of most Martian meteorites were sulfide-undersaturated. • Martian mantle and core have a low sulfur content. • Low Te/PGE ratios in Martian meteorites reflect a strongly volatile element-depleted Martian late veneer.
提供机构：
TRR170-DB
创建时间：
2020-11-13
