Importance of mineralogical spectroscopy on planetary exploration.

Author:

HIRAO Naohisa

Publisher

Japan Association of Mineralogical Sciences

Subject

Economic Geology,Geochemistry and Petrology

Reference78 articles.

1. Adams, J.B. (1974): Visible and near-infrared diffuse reflectance spectra of pyroxenes as applied to remote sensing of solid objects in the solar system. J. Geophys. Res., 79, 4829-4836.

2. Adams, J.B. and Goulland, L.H. (1978): Plagioclase feldspars: Visible and near-infrared diffuse reflectance spectra as applied to remote sensing (abstract). Lunar Planet. Sci. Conf. 9, 1-3.

3. Allen, C.C., Morris, R.V., Lauer, H.V.Jr. and Mckay, D.S. (1993): Microscopic iron met al on glass and minerals—A tool for studying regolith maturity. ICARUS, 104, 291-300.

4. Bell, P.M. and Mao, H.K. (1973): Optical and chemical analysis of iron in Luna 20 plagioclase. Geochim. Cosmochim. Acta, 37, 755-759.

5. Bell, J.F., Davis, D.R., Hartman, W.K. and Gaffey, M.J. (1989): Asteroids: The big picture. In Asteroids II (Binzel, R.P. et al. Eds.). Univ. Arizona Press, Tucson, Arizona, 921-945.

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