Thermal Metamorphism in L Chondrites: Implications of Percent Mean Deviation in Olivine and Pyroxene

Details Thermal Metamorphism in L Chondrites: Implications of Percent Mean Deviation in Olivine and Pyroxene Thermal Metamorphism in L Chondrites: Implications of Percent Mean Deviation in Olivine and Pyroxene

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.2033m&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.2033

Physics

Scientific paper

We are developing a new technique to quickly and accurately measure the
homogeneity of olivines and pyroxenes in a suite of L-chondrites. We are
able to determine the average wt% Fe of minerals in Gold Basin (L4).

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