Axtell and Allende: A Mössbauer Spectroscopic Study

Details Axtell and Allende: A Mössbauer Spectroscopic Study Axtell and Allende: A Mössbauer Spectroscopic Study

Mar 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000m%26ps...35..431h&link_type=abstract

Meteoritics & Planetary Science, vol. 35, no. 2, pp. 431-434 (2000).

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Mössbauer spectra showed the CV3 oxidized subgroup meteorites Allende and Axtell to be similar in olivine content and a surprising lack of pronounced magnetic components, but different in Fe3+ phases. One atypical Allende sample showed an 8% area under the curve for magnetite, still less than a reported value for a CV3 reduced subgroup member. Allende's unusual Fe3+ spectral region distinguishes it from most other stony meteorites and is difficult to fit to known mineral parameters.

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