The Mineralogy of Simulated Martian Basalt Alteration: Clues from Smectite Assemblages
收藏NIAID Data Ecosystem2026-05-10 收录
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Our study addresses a critical gap in the paleoenvironmental reconstruction of Mars by moving beyond the limitations of interpreting individual mineral phases. Through systematic hydrothermal experiments simulating a broad pH range (pH=4-13), we investigate the formation of smectite-associated mineral assemblages and their implications for Martian aqueous environments.
创建时间：
2025-09-16
