Possible Formation of IVA Irons by Impact Melting and Reduction of L-LL Chondrite Materials

Details Possible Formation of IVA Irons by Impact Melting and Reduction of L-LL Chondrite Materials Possible Formation of IVA Irons by Impact Melting and Reduction of L-LL Chondrite Materials

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1511w&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1511

Computer Science

Scientific paper

The oxygen-isotope composition of silicates in IVA irons indicates an
origin from L-LL chondritic materials. This requires appreciable
reduction. We suggest that melting and reduction resulted from an impact
onto a porous primitive chondritic body.

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