Laboratory Shock Experiments on Basalt — Iron Sulfate Mixes at ~40-50 GPa and Their Relevance to the Martian Regolith Component Present in Shergottites

Details Laboratory Shock Experiments on Basalt — Iron Sulfate Mixes at ~40-50 GPa and Their Relevance to the Martian Regolith Component Present in Shergottites Laboratory Shock Experiments on Basalt — Iron Sulfate Mixes at ~40-50 GPa and Their Relevance to the Martian Regolith Component Present in Shergottites

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2102r&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2102

Physics

1

Scientific paper

By conducting laboratory shock experiments, we demonstrate the
plausibility of iron sulfate reduction to sulfides in martian meteorites
by shock.

Affiliated with

Also associated with

No associations

Rating

Laboratory Shock Experiments on Basalt — Iron Sulfate Mixes at ~40-50 GPa and Their Relevance to the Martian Regolith Component Present in Shergottites does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Laboratory Shock Experiments on Basalt — Iron Sulfate Mixes at ~40-50 GPa and Their Relevance to the Martian Regolith Component Present in Shergottites, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Laboratory Shock Experiments on Basalt — Iron Sulfate Mixes at ~40-50 GPa and Their Relevance to the Martian Regolith Component Present in Shergottites will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1040886