Chromite composition in relation to chemistry and texture of ordinary chondrites

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Scientific paper

Analyses of chromite from forty-six ordinary chondrites were made using electron microprobe techniques. Two correlations were found between chromite composition and chondrite classification. First, the composition of chromite in "equilibrated" ordinary chondrites changes in an orderly fashion from H to L to LL groups, in accordance with changes in olivine and orthopyroxene compositions. Second, within the three major ordinary chondrite groups, chromite composition is related to petrographic subgroup. The observed trends are consistent with either a metamorphic or primary igneous origin of chondrites of different petrographic subgroups. Notable amounts of vanadium were found in all analyzed chromites. Vanadium is enriched in chromite in comparison to the bulk meteorite by a factor of 70. The portion of the total vanadium combined in chromite increases from lower- to higher-numbered subgroups due to an increase in total chromite content of the meteorites.

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