Trace Elements Abundances vs. Closure Temperature in Orthopyroxenes from Howardites

Details Trace Elements Abundances vs. Closure Temperature in Orthopyroxenes from Howardites Trace Elements Abundances vs. Closure Temperature in Orthopyroxenes from Howardites

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1146d&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1146

Physics

Scientific paper

Trace elements abundances, measured by LAM-ICP-MS on orthopyroxene from
Kapoeta, Old Homestead 001 and Hughes 004 howardites, were related with
the closure temperature of Fe-Mg exchange reaction.

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