Saturation magnetization measurements of carbonaceous chondrites

Details Saturation magnetization measurements of carbonaceous chondrites Saturation magnetization measurements of carbonaceous chondrites

Mar 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986metic..21....1h&link_type=abstract

Meteoritics (ISSN 0026-1114), vol. 21, March 31, 1986, p. 1-22. Research supported by the Texas A & M University.

Computer Science

6

Carbonaceous Chondrites, Magnetic Measurement, Magnetization, Meteoritic Composition, Faraday Effect, Iron, Magnetite, Saturation, Meteorites, Carbonaceous Chondrites, Stony Meteorites, Techniques, Saturation Magnetization, Samples, Meteorite, Magnetite, Composition, Cm2 Chondrites, Cv3 Chondrites, Abundance, Concentration, Iron, Metal, Comparisons, Procedure, Ci Chondrites, Antarctic Meteorites, Allan Hills Meteorites, Electron Microscopy, Sem, Photomicrographs, Co3 Chondrites, C5 Chondrites, Catalog

Scientific paper

The saturation magnetization of some carbonaceous chondrites was studied using a Faraday balance. The authors present measurements on the magnetite contents of some CM2, CV3 and a CV5 chondrites. The method was also used to measure the content of metallic nickel-iron in Ornans, 3.4±0.3%. Of the CM2 chondrites examined, only Bells, Essebi and Haripura had magnetite contents over about 1% by weight. A number of CV chondrites have magnetite between 2.3 and 13%, with little or no metallic iron. Leoville and Vigarano contain both magnetite and metallic iron, complicating the saturation magnetization results. Arch and Allende have very little metallic iron or magnetite, probably <1% of either.

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