Aqueous Alteration of Granitoid-bearing Terrains in Northwest Syrtis Major, Mars: Evidence for Alteration Gradients in a Hydrothermal Environment

Details Aqueous Alteration of Granitoid-bearing Terrains in Northwest Syrtis Major, Mars: Evidence for Alteration Gradients in a Hydrothermal Environment Aqueous Alteration of Granitoid-bearing Terrains in Northwest Syrtis Major, Mars: Evidence for Alteration Gradients in a Hydrothermal Environment

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2194s&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2194

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Scientific paper

We investigate a mineral assemblage in NW Syrtis Major consisting of
hydrated (phyllosilicates, hydrated silica, and zeolites) and granitoid
(quartz and plagioclase) materials and assess its origin as a
plutonically driven hydrothermal system.

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