Moessbauer study of the Putinga chondrite

Details Moessbauer study of the Putinga chondrite Moessbauer study of the Putinga chondrite

Jan 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988phys...37..185d&link_type=abstract

Physica Scripta (ISSN 0031-8949), vol. 37, no. 1, Jan. 1988, p. 185-187. Research supported by the Coordenacao do Aperfeicoament

Physics

Absorption Spectra, Chondrites, Meteoritic Composition, Meteoritic Microstructures, Mossbauer Effect, Crystal Structure, Kamacite, Olivine, Pyroxenes, Troilite

Scientific paper

The Putinga meteorite, classified as an L-6 ordinary chondrite, was studied by 57Fe Mössbauer spectroscopy at 300K and 80K. The iron mineral phases present in the Putinga meteorite were determined to be olivine, orthopyroxene, troilite, paramagnetic taenite, kamacite and an Fe3+-compound. It is suggested that the Fe3+-compound has originated from oxidation of the sample in the earth atmosphere.

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