K-Ar ages of Lafayette weather products - Evidence for near-surface liquid water on Mars in the last few hundred million years

Computer Science

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Mars Surface, Rare Gases, Weathering, Water, Meteoritic Composition, Mars Atmosphere, Magma, Krypton Isotopes, Argon Isotopes, Chronology

Scientific paper

Results of studies of the K-Ar ages of 19 hand-picked samples of Lafayette iddingsite are presented. It is found that, since many samples have ages far greater than the possible terrestrial age of this meteorite, the iddingsite must be preterrestrial (i.e., Martian). The samples to not hall have the same apparent K-Ar age. This could either reflect multiple episodes of iddingsite formation or differing degrees of partial loss. The weathering products in the Lafayette meteorite formed as a result of the action of near-surface liquid water on Mars in one or more events not more than 700 Ma ago.

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