Mixed Hydrothermal Fluids and the Origin of the Martian Soil: A New Quantitative Model

Details Mixed Hydrothermal Fluids and the Origin of the Martian Soil: A New Quantitative Model Mixed Hydrothermal Fluids and the Origin of the Martian Soil: A New Quantitative Model

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1262n&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1262

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Scientific paper

A combination of neutral-chloride hydrothermal fluids (providing Cl) and
acid-sulfate fluids (providing S) can quantitatively explain the
abundances of S, Cl, and other mobile elements in the soil, but not the
Fe in soil magnetic minerals.

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