Hydraulic Properties Control Phyllosilicate and Zeolite Formation in Basaltic Tuffs: Implications for Detection and Alteration Processes on Mars

Details Hydraulic Properties Control Phyllosilicate and Zeolite Formation in Basaltic Tuffs: Implications for Detection and Alteration Processes on Mars Hydraulic Properties Control Phyllosilicate and Zeolite Formation in Basaltic Tuffs: Implications for Detection and Alteration Processes on Mars

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1226s&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1226

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Scientific paper

Basaltic hydrovolcanic tuffs from central Oregon illustrate how primary
porosity and permeability control hydrothermal fluid flow and alteration
assemblages.

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