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  1. 1
    Three-stage formation of cap carbonates after Marinoan snowball glaciation consistent with depositional timescales and geochemistry

    Three-stage formation of cap carbonates after Marinoan snowball glaciation consistent with depositional timescales and geochemistry by Trent B. Thomas, David C. Catling

    Published 2024-08-01
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  2. 2
    Constraints on the Size and Composition of the Ancient Martian Atmosphere from Coupled CO2–N2–Ar Isotopic Evolution Models

    Constraints on the Size and Composition of the Ancient Martian Atmosphere from Coupled CO2–N2–Ar Isotopic Evolution Models by Trent B. Thomas, Renyu Hu, Daniel Y. Lo

    Published 2023-01-01
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