Mossbauer study of the Allende meteorite

Details Mossbauer study of the Allende meteorite Mossbauer study of the Allende meteorite

Mar 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984metic..19...25o&link_type=abstract

Meteoritics (ISSN 0026-1114), vol. 19, March 31, 1984, p. 25-27.

Computer Science

7

Carbonaceous Chondrites, Iron Meteorites, Meteoritic Composition, Mineralogy, Mossbauer Effect, Olivine, Meteorites, Allende, Carbonaceous Chondrites, Chemistry, Mineralogy, Mossbauer Spectroscopy, Nuclear Gamma Resonance, Ngr, Iron, Composition, Spectra, Comparisons, Magnetic Properties, Patterns, Samples, Meteorite

Scientific paper

A room temperature spectrum of a Moessbauer investigation of the Allende III carbonaceous chondrite is presented. Analysis demonstrates that the iron minerals are predominantly olivine, and that there exists a small quantity of a phyllosilicate or goethite. The magnitude of the isomer shift relative to iron foil (1.43 + or - .01 mm/s) for the olivine shows iron to be in the Fe(2) state. Quadrupole splitting of the olivine is 2.92 + or - .01 m/s. Nothing suggests appreciable quantities of ferromagnetic materials.

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