Paired Fine Grained, Permafic Olivine-Phyric Shergottites Northwest Africa 2990/5960/6234/6710: Trace Element Evidence for a New Type of Martian Mantle Source or Complex Lithospheric Assimilation Processes

Details Paired Fine Grained, Permafic Olivine-Phyric Shergottites Northwest Africa 2990/5960/6234/6710: Trace Element Evidence for a New Type of Martian Mantle Source or Complex Lithospheric Assimilation Processes Paired Fine Grained, Permafic Olivine-Phyric Shergottites Northwest Africa 2990/5960/6234/6710: Trace Element Evidence for a New Type of Martian Mantle Source or Complex Lithospheric Assimilation Processes

Sep 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011m%26psa..74.5232i&link_type=article

74th Annual Meeting of the Meteoritical Society, held August 8-12, 2011 in London, UK. Published in Meteoritics and Planetary S

Physics

Scientific paper

Not Available

Affiliated with

Also associated with

No associations

Rating

Paired Fine Grained, Permafic Olivine-Phyric Shergottites Northwest Africa 2990/5960/6234/6710: Trace Element Evidence for a New Type of Martian Mantle Source or Complex Lithospheric Assimilation Processes 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 Paired Fine Grained, Permafic Olivine-Phyric Shergottites Northwest Africa 2990/5960/6234/6710: Trace Element Evidence for a New Type of Martian Mantle Source or Complex Lithospheric Assimilation Processes, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Paired Fine Grained, Permafic Olivine-Phyric Shergottites Northwest Africa 2990/5960/6234/6710: Trace Element Evidence for a New Type of Martian Mantle Source or Complex Lithospheric Assimilation Processes will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1408557