Comparative Cooling Rates of Nakhlites as Inferred from Iron-Magnesiumand Calcium Zoning of Olivines

Details Comparative Cooling Rates of Nakhlites as Inferred from Iron-Magnesiumand Calcium Zoning of Olivines Comparative Cooling Rates of Nakhlites as Inferred from Iron-Magnesiumand Calcium Zoning of Olivines

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1343m&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1343

Physics

4

Scientific paper

We estimated cooling rates of nakhlites by using Fe-Mg and Ca zoning
profiles of olivines. The results suggest that NWA817 cooled near the
surface, and Lafayette was located deeper than 30 m. Nakhla and
Governador Valadares appear intermediate.

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