Hydrothermal Alteration of 2.7 Ga Basaltic Andesites and Implications for Past Fluid-Rock Interactions on Mars

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Scientific paper

A ca. 2701 Ma outcrop of greenschist-facies metabasites in the Abitibi
greenstone belt of Canada provides an analogue for studying Earth and
martian-like hydrothermal fluid interactions with mafic lavas at sites
possibly hosting microorganisms.

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