Secondary Minerals in the Nakhlites Formed at Varying Depths in an Impact Hydrothermal Cell

Details Secondary Minerals in the Nakhlites Formed at Varying Depths in an Impact Hydrothermal Cell Secondary Minerals in the Nakhlites Formed at Varying Depths in an Impact Hydrothermal Cell

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1407c&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1407

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Scientific paper

Amorphous gel and Fe-smectite within the nakhlites show compositional
fractionation consistent with varying depths of origin. They formed from
neutral pH and progressively oxidised fluids during an impact
hydrothermal/evaporation event.

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