Experimental Simulation of Magmatic Hydrothermal Activity on Mars: I. High Temperature Alteration in the Presence of a Cl-and S-enriched Fluid

Details Experimental Simulation of Magmatic Hydrothermal Activity on Mars: I. High Temperature Alteration in the Presence of a Cl-and S-enriched Fluid Experimental Simulation of Magmatic Hydrothermal Activity on Mars: I. High Temperature Alteration in the Presence of a Cl-and S-enriched Fluid

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1774n&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1774

Computer Science

Scientific paper

Experimental alteration of a partly crystallized Humphrey basalt by
Cl-and S- fluid exsolved from a magma of Backstay composition at
mid-crustal levels produced a martian amphibolite.

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