Observations on the Fe-Si-Mg relationship in chondrites

Details Observations on the Fe-Si-Mg relationship in chondrites Observations on the Fe-Si-Mg relationship in chondrites

Jul 1965

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1965gecoa..29..801a&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 29, Issue 7, p. 801-806.

Physics

8

Scientific paper

The Fe-Si-Mg relationship in chondrites, as represented on a triangular diagram and Si-Mg fractionation are considered. The possibility of utilizing some of these relationships for chondrite classification and assignment are discussed. Though Si-Mg fractionation between enstatite-chondrites, carbonaceous chondrites (including the olivine-pigeonite group) and the common chondrites (olivine-bronzite and olivine-hypersthene) is now well established, it has not been possible to ascertain whether fractionation between the olivine-bronzite and olivine-hypersthene chondrites has taken place; present evidence indicates that there might be slight fractionation. References

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