The Cooling Rate of Several Olivine-Phyric Shergottites on the basis of Fe-Mg Zoning in Olivine

Details The Cooling Rate of Several Olivine-Phyric Shergottites on the basis of Fe-Mg Zoning in Olivine The Cooling Rate of Several Olivine-Phyric Shergottites on the basis of Fe-Mg Zoning in Olivine

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1554m&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1554

Physics

Scientific paper

We have developed a model to calculate the cooling rate and burial depth
by using the Fe-Mg zoning of olivine and applied this model to
calculating the cooling rate and burial depth for several olivine-phyric
shergottites.

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