Petrologic, Elemental and Multi-Isotopic Characterization of Permafic Olivine-Phyric Shergottite Northwest Africa 5789: A Primitive Magma Derived from Depleted Martian Mantle

Details Petrologic, Elemental and Multi-Isotopic Characterization of Permafic Olivine-Phyric Shergottite Northwest Africa 5789: A Primitive Magma Derived from Depleted Martian Mantle Petrologic, Elemental and Multi-Isotopic Characterization of Permafic Olivine-Phyric Shergottite Northwest Africa 5789: A Primitive Magma Derived from Depleted Martian Mantle

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1547i&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1547

Mathematics

Logic

2

Scientific paper

We report on an extensive petrological-chemical study of a very
primitive depleted shergottite, which is similar in many (but not all)
respects to Yamato 980459/98497.

Affiliated with

Also associated with

No associations

Rating

Petrologic, Elemental and Multi-Isotopic Characterization of Permafic Olivine-Phyric Shergottite Northwest Africa 5789: A Primitive Magma Derived from Depleted Martian Mantle 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 Petrologic, Elemental and Multi-Isotopic Characterization of Permafic Olivine-Phyric Shergottite Northwest Africa 5789: A Primitive Magma Derived from Depleted Martian Mantle, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Petrologic, Elemental and Multi-Isotopic Characterization of Permafic Olivine-Phyric Shergottite Northwest Africa 5789: A Primitive Magma Derived from Depleted Martian Mantle will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-888613