Ureilites as the Moderate-SiO2 Residue of Basaltic Melt Removal from a Diverse Aggregate of SiO2-Rich Chondritic Parent Materials

Details Ureilites as the Moderate-SiO2 Residue of Basaltic Melt Removal from a Diverse Aggregate of SiO2-Rich Chondritic Parent Materials Ureilites as the Moderate-SiO2 Residue of Basaltic Melt Removal from a Diverse Aggregate of SiO2-Rich Chondritic Parent Materials

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2769w&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2769

Computer Science

Scientific paper

Mass-balance modeling for average ureilite as an anatexis residue
indicates the ureilite starting materials had far higher SiO2/FeO ratio
in comparison to any known type of carbonaceous chondrite.

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