Evidence for Tectonically Controlled Hydrothermal Fluid Flow in Relay Zones on Mars from Early HiRISE Images

Details Evidence for Tectonically Controlled Hydrothermal Fluid Flow in Relay Zones on Mars from Early HiRISE Images Evidence for Tectonically Controlled Hydrothermal Fluid Flow in Relay Zones on Mars from Early HiRISE Images

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1788d&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

1

Scientific paper

Preliminary observations show outflow channels sourced from relays
between fault segments. New high resolution data from HiRISE on MRO
reveals high density bleached joint sets proximal to a fault relay zone
in Melas Chasm.

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