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Visible/near-infrared spectral diversity from in situ observations of the Bagnold Dune Field sands in Gale Crater, Mars

As part of the Bagnold Dune campaign conducted by Mars Science Laboratory rover Curiosity, visible/near-infrared reflectance spectra of dune sands were acquired using Mast Camera (Mastcam) multispectral imaging (445-1013nm) and Chemistry and Camera (ChemCam) passive point spectroscopy (400-840nm). By comparing spectra from pristine and rover-disturbed ripple crests and troughs within the dune field, and through analysis of sieved grain size fractions, constraints on mineral segregation from grain sorting could be determined. In general, the dune areas exhibited low relative reflectance, a weak similar to 530nm absorption band, an absorption band near 620nm, and a spectral downturn after similar to 685nm consistent with olivine-bearing sands. The finest grain size fractions occurred within ripple troughs and in the subsurface and typically exhibited the strongest similar to 530nm bands, highest relative reflectances, and weakest red/near-infrared ratios, consistent with a combination of crystalline and amorphous ferric materials. Coarser-grained samples were the darkest and bluest and exhibited weaker similar to 530nm bands, lower relative reflectances, and stronger downturns in the near-infrared, consistent with greater proportions of mafic minerals such as olivine and pyroxene. These grains were typically segregated along ripple crests and among the upper surfaces of grain flows in disturbed sands. Sieved dune sands exhibited progressive decreases in reflectance with increasing grain size, as observed in laboratory spectra of olivine size separates. The continuum of spectral features observed between the coarse- and fine-grained dune sands suggests that mafic grains, ferric materials, and air fall dust mix in variable proportions depending on aeolian activity and grain sorting.

Identiferoai:union.ndltd.org:arizona.edu/oai:arizona.openrepository.com:10150/626566
Date12 1900
CreatorsJohnson, Jeffrey R., Achilles, Cherie, Bell, James F., Bender, Steve, Cloutis, Edward, Ehlmann, Bethany, Fraeman, Abigail, Gasnault, Olivier, Hamilton, Victoria E., Le Mouélic, Stéphane, Maurice, Sylvestre, Pinet, Patrick, Thompson, Lucy, Wellington, Danika, Wiens, Roger C.
ContributorsUniv Arizona, Dept Geosci, The Johns Hopkins University Applied Physics Laboratory; Laurel Maryland USA, Department of Geoscience; University of Arizona; Tucson Arizona USA, School of Earth and Space Exploration; Arizona State University; Tempe Arizona USA, Planetary Science Institute; Tucson Arizona USA, Department of Geography; University of Winnipeg; Winnipeg Manitoba Canada, Jet Propulsion Laboratory; California Institute of Technology; Pasadena California USA, Jet Propulsion Laboratory; California Institute of Technology; Pasadena California USA, Institut de Recherche en Astrophysique et Planetologie; Université de Toulouse, CNRS; Toulouse France, Southwest Research Institute; Boulder Colorado USA, Laboratoire de Planétologie et Géodynamique; Université de Nantes; Nantes France, Institut de Recherche en Astrophysique et Planetologie; Université de Toulouse, CNRS; Toulouse France, Institut de Recherche en Astrophysique et Planetologie; Université de Toulouse, CNRS; Toulouse France, Planetary and Space Science Centre; University of New Brunswick; Fredericton New Brunswick Canada, School of Earth and Space Exploration; Arizona State University; Tempe Arizona USA, Los Alamos National Laboratory; Los Alamos New Mexico USA
PublisherAMER GEOPHYSICAL UNION
Source SetsUniversity of Arizona
LanguageEnglish
Detected LanguageEnglish
TypeArticle
Rights©2017. American Geophysical Union. All Rights Reserved.
Relationhttp://doi.wiley.com/10.1002/2016JE005187

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