Constraints on olivine-rich rock types on the Moon as observed by Diviner and M3 : Implications for the formation of the lunar crust

Author:

Arnold J. A.12,Glotch T. D.1,Lucey P. G.3,Song E.4,Thomas I. R.25,Bowles N. E.2,Greenhagen B. T.6

Affiliation:

1. Department of Geosciences; Stony Brook University; Stony Brook New York USA

2. Atmospheric, Oceanic and Planetary Physics, Department of Physics; Oxford University; Oxford UK

3. Hawaii Institute of Geophysics and Planetology; University of Hawaii; Honolulu Hawaii USA

4. Jet Propulsion Laboratory; Pasadena California USA

5. Royal Belgian Institute for Space Aeronomy; Brussels Belgium

6. The Johns Hopkins University Applied Physics Laboratory; Laurel Maryland USA

Funder

Diviner Lunar Radiometer Extended Mission science investigation

RIS4E Solar System Exploration Research Virtual Institute investigation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference101 articles.

1. Plagioclase feldspars-Visible and near infrared diffuse reflectance spectra as applied to remote sensing;Adams;Lunar Planet. Sci. Conf. Proc.,1978

2. Electronic spectra of pyroxenes and interpretation of telescopic spectral reflectivity curves of the Moon;Adams;Lunar Planet. Sci. Conf. Proc.,1972

3. Effects of shock-loading on the reflectance spectra of plagioclase, pyroxene, and glass;Adams;Lunar Planet. Sci. Conf. Proc.,1979

4. Spectral mixture modeling: A new analysis of rock and soil types at the Viking Lander 1 site;Adams;J. Geophys. Res.,1986

5. Spectral reflectance and emittance of particulate materials. 2: Application and results;Aronson;Appl. Opt.,1973

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