Stable Isotope Composition of Carbonates Formed in Low-Temperature Terrestrial Environments as Martian Analogs

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Scientific paper

We report the C and O isotope composition of carbonate minerals that
formed in two low-temperature environments. Results show an overall
depletion of ^18O and ^13C as a function of the extent of meteoric
diagenesis. These data are used as analogs to carbonates that have been
found in ALH84001.

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