Evidence for Parent-Body Thermal-Metamorphism of CO3 Chondrite by Analyzing Fe-Mg Zoning of Olivine

Details Evidence for Parent-Body Thermal-Metamorphism of CO3 Chondrite by Analyzing Fe-Mg Zoning of Olivine Evidence for Parent-Body Thermal-Metamorphism of CO3 Chondrite by Analyzing Fe-Mg Zoning of Olivine

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1156m&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1156

Physics

Scientific paper

We studied whether thermal metamorphism of Y-791717 CO3.6 chondrite
occurred in the parent body or in the primitive solar nebula by fitting
the calculated Fe zoning of olivine to observed one. The result for the
600°-1000°C range shows the best fit.

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