Spectral chemistry of green glass-bearing 15426 regolith.

Details Spectral chemistry of green glass-bearing 15426 regolith. Spectral chemistry of green glass-bearing 15426 regolith.

Jan 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983jgr....88..221b&link_type=abstract

Journal of Geophysical Research, Vol. 88, Suppl., p. B221 - B228

Physics

4

Moon Samples:Chemistry

Scientific paper

The detection of appreciable concentrations of ferric iron in a synthetic green glass equilibrated at an oxygen fugacity of 10-11 atm prompted a Mössbauer spectral study of pristine emerald-green glass spherules carefully handpicked from regolith sample 15426. No Fe3+ ions were detected in this lunar sample or in a synthetic green glass simulant equilibrated at fO2 = 10-14atm, suggesting that the green glass clods in rock 15426 formed under conditions of correspondingly low oxygen fugacities. The Mössbauer spectra indicated the presence of olivine crystallites in the lunar emerald green glass spherules.

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