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Effects of Palagonitic Dust Coatings on Visible, Near-IR, and Mossbauer Spectra of Rocks and Minerals: Implication for Mineralogical Remote Sensing of MarsVisible, near-IR, and Mossbauer measurements on dust coated rocks and minerals show that a 300 5m thick layer is required to obscure the substrate for VNIR measurements and that a greater than 2000-micron-thick layer is required to obscure the substrate for Mossbauer measurements. Additional information is contained in the original extended abstract.
Document ID
20010045427
Document Type
Conference Paper
Authors
Morris, R.
(NASA Johnson Space Center Houston, TX United States)
Graff, T. G.
(Arizona State Univ. Tempe, AZ United States)
Shelfer, T. D.
(NASA Johnson Space Center Houston, TX United States)
Bell, J. F., III
(Cornell Univ. Ithaca, NY United States)
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Publication Information
Publication: Lunar and Planetary Science XXXII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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