Origin of the Ungrouped Achondrite NWA 4518: Mineralogy and Geochemistry of FeNi-Metal

Details Origin of the Ungrouped Achondrite NWA 4518: Mineralogy and Geochemistry of FeNi-Metal Origin of the Ungrouped Achondrite NWA 4518: Mineralogy and Geochemistry of FeNi-Metal

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1291l&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1291

Computer Science

Scientific paper

Ungrouped achondrite NWA 4518 is an ultramafic breccia with abundant
siderophile rich IIA-like metal. Its silicate chemistry is similar to
that of WINs, HEDs, and silicate inclusions of IIE irons. Oxygen
isotopic composition is nearby IAB-IIICD-WIN.

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