Identical Origin for Halide and Sulfate Efflorescences on Meteorite Finds and Sulfate Veins in Orgueil

Details Identical Origin for Halide and Sulfate Efflorescences on Meteorite Finds and Sulfate Veins in Orgueil Identical Origin for Halide and Sulfate Efflorescences on Meteorite Finds and Sulfate Veins in Orgueil

Jan 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000lpico.997...95z&link_type=abstract

Workshop on Extraterrestrial Materials from Cold and Hot Deserts, p. 95

Physics

Meteorites, Halides, Sulfates, Asteroids, Deserts

Scientific paper

Halide and sulfate efflorescences are common on meteorite finds,
especially those from cold deserts. Meanwhile, the late-stage sulfate
veins in Orgueil are universally accepted as having originated by the
action of late-stage high fO2 aqueous alteration on an asteroid. I
suggest here that these phenomena have essentially the same origin.

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