New data on the forms of iron found in the Luna-16 regolith, obtained using Moessbauer spectroscopy

Details New data on the forms of iron found in the Luna-16 regolith, obtained using Moessbauer spectroscopy New data on the forms of iron found in the Luna-16 regolith, obtained using Moessbauer spectroscopy

Aug 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989geokh.....1170v&link_type=abstract

Geokhimiia (ISSN 0016-7525), Aug. 1989, p. 1170-1175. In Russian.

Computer Science

Iron Compounds, Lunar Soil, Mossbauer Effect, Regolith, Lunar Geology, Lunik 16 Lunar Probe, Spectrum Analysis

Scientific paper

Results are presented from a detailed analysis of the Moessbauer spectra of the smallest (not greater than 80 microns) fraction of the Luna-16 regolith, using difference spectra to determine the mineral forms of iron in this regolith. The percentages of Fe found in various minerals were as follows: olivine, 19.0; pyroxene, 32.0; glass, 18.2; ilmenite, 11.2; ulvoespinel, 5.6; and metallic Fe, 14.0. Conclusions concerning the maturity of the regolith were drawn, based on the ratio of structured (olivine + pyroxene) and unstructured (glass) forms of iron.

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