Pre-terrestrial oxidation products in carbonaceous meteorites identified by Mossbauer spectroscopy

Details Pre-terrestrial oxidation products in carbonaceous meteorites identified by Mossbauer spectroscopy Pre-terrestrial oxidation products in carbonaceous meteorites identified by Mossbauer spectroscopy

Jun 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991pggp.rept..256b&link_type=abstract

In NASA, Washington, Reports of Planetary Geology and Geophysics Program, 1990 p 256-258 (SEE N92-10728 01-91)

Physics

Geophysics

Carbonaceous Chondrites, Carbonaceous Meteorites, Iron, Oxidation, Spectra, Spectroscopy, Hydroxides, Magnetite, Oxides, Silicates

Scientific paper

The occurrence of ferric bearing assemblages, comprising phyllosilicates, oxide hydroxides and magnetite, in carbonaceous chondrites (CC) indicates that these meteorites underwent pre-terrestrial, sub-aqueous oxidation reactions. Reported here are results of a Mossbauer spectral study of a suite of CC demonstrating that a variety of ferrous and ferric bearing phases may be distinguished in different classes of this meteorite type.

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