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Part I - Theory of Remote Compositional Analysis Techniques and Laboratory Measurements

Published online by Cambridge University Press:  15 November 2019

Janice L. Bishop
Affiliation:
SETI Institute, California
James F. Bell III
Affiliation:
Arizona State University
Jeffrey E. Moersch
Affiliation:
University of Tennessee, Knoxville
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Remote Compositional Analysis
Techniques for Understanding Spectroscopy, Mineralogy, and Geochemistry of Planetary Surfaces
, pp. 1 - 258
Publisher: Cambridge University Press
Print publication year: 2019

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References

References

Amthauer, G. & Rossman, G.R. (1984) Mixed valence of iron in minerals with cation clusters. Physics and Chemistry of Minerals, 11, 3751.CrossRefGoogle Scholar
Aronson, J.R., Bellotti, L.H., Eckroad, S.W., Emslie, A.G., McConnell, R.K., & Thüna, P.C. (1970) Infrared spectra and radiative thermal conductivity of minerals at high temperature. Journal of Geophysical Research, 75(17), 34433456.CrossRefGoogle Scholar
Baratoux, D., Toplis, M.J., Monnereau, M., & Sautter, V. (2013) The petrological expression of early Mars volcanism. Journal of Geophysical Research, 118, 5964.Google Scholar
Bell, P.M. & Mao, H.K. (1973) Optical and chemical analysis of iron in Luna 20 plagioclase. Geochimica et Cosmochimica Acta, 37, 755759.CrossRefGoogle Scholar
Berg, B.L., Cloutis, E.A., Beck, P., et al. (2016) Reflectance spectroscopy (0.35–25 µm) of ammonium-bearing minerals and comparison to Ceres family asteroids. Icarus, 265, 218237.CrossRefGoogle Scholar
Bishop, J.L. & Murad, E. (1996) Schwertmannite on Mars? Spectroscopic analyses of schwertmannite, its relationship to other ferric minerals, and its possible presence in the surface material on Mars. In: Mineral spectroscopy: A tribute to Roger G. Burns. Special publication (Geochemical Society). No. 5. Geochemical Society, Houston, TX, 337358.
Bishop, J.L., Dyar, M.D., Lane, M.D., & Banfield, J.F. (2004) Spectral identification of hydrated sulfates on Mars and comparison with acidic environments on Earth. International Journal of Astrobiology, 3, 275285.CrossRefGoogle Scholar
Bishop, J.L., Perry, K.A., Dyar, M.D., et al. (2013) Coordinated spectral and XRD analyses of magnesite-nontronite-forsterite mixtures and implications for carbonates on Mars. Journal of Geophysical Research, 118, 635650.Google Scholar
Burns, R.G. (1981) Intervalence transitions in mixed valence minerals of iron and titanium. Annual Review of Earth and Planetary Sciences, 9, 345383.CrossRefGoogle Scholar
Burns, R.G. (1993) Mineralogical applications of crystal field theory. Cambridge University Press, Cambridge.CrossRefGoogle Scholar
Burns, R.G. & Vaughan, D.J. (1975) 2 – Polarized Electronic Spectra. In: Infrared and Raman spectroscopy of lunar and terrestrial minerals (Karr, C., ed.). Academic Press, New York, 3972.CrossRefGoogle Scholar
Cannon, K.M., Mustard, J.F., Parman, S.W., Sklute, E.C., Dyar, M.D., & Cooper, R.F. (2017) Spectral properties of martian and other planetary glasses and their detection in remotely sensed data. Journal of Geophysical Research, 122, 249268.Google Scholar
Carlson, R.W., Smythe, W.D., Lopes-Gautier, R.M.C., et al. (1997) The distribution of sulfur dioxide and other infrared absorbers on the surface of Io. Geophysical Research Letters, 24, 24792482.CrossRefGoogle Scholar
Cheek, L.C. (2014) Foundations of lunar highland crustal mineralogy derived from remote sensing and laboratory spectroscopy of plagioclase-dominated Materials. Brown University Earth, Environmental and Planetary Sciences Theses and Dissertations.
Chemtob, S.M., Nickerson, R.D., Morris, R.V., Agresti, D.G., & Catalano, J.G. (2015) Synthesis and structural characterization of ferrous trioctahedral smectites: Implications for clay mineral genesis and detectability on Mars. Journal of Geophysical Research, 120, 11191140.Google Scholar
Cloutis, E.A., Sunshine, J.M., & Morris, R.V. (2004) Spectral reflectance-compositional properties of spinels and chromites: Implications for planetary remote sensing and geothermometry. Meteoritics and Planetary Science, 39, 545565.CrossRefGoogle Scholar
Cloutis, E.A., Hawthorne, F.C., Mertzman, S.A., et al. (2006) Detection and discrimination of sulfate minerals using reflectance spectroscopy. Icarus, 184, 121157.CrossRefGoogle Scholar
Cotton, F.A. (1990) Chemical applications of group theory, 3rd edn. Wiley-Interscience, New York.Google Scholar
DeMeo, F.E., Binzel, R.P., Slivan, S.M., & Bus, S.J. (2009) An extension of the Bus asteroid taxonomy into the near-infrared. Icarus, 202, 160180.CrossRefGoogle Scholar
De Sanctis, M.C., Ammannito, E., Capria, M.T., et al. (2012) Spectroscopic characterization of mineralogy and its diversity across Vesta. Science, 336, 697.CrossRefGoogle ScholarPubMed
Dowty, E.C. & Clark, J.R. (1973) Crystal structure refinement and visible-region absorption spectra of a Ti3+ fassaite from the Allende meteorite. American Mineralogist, 58, 230242.Google Scholar
Eckert, B. & Steudel, R. (2003) Molecular spectra of sulfur molecules and solid sulfur allotropes. In: Elemental sulfur and sulfur-rich compounds II (Steudel, R., ed.). Springer, Berlin, Heidelberg, 3198.Google Scholar
Ehlmann, B.L. & Edwards, C.S. (2014) Mineralogy of the martian surface. Annual Review of Earth and Planetary Sciences, 42, 291315.CrossRefGoogle Scholar
Fraeman, A.A., Arvidson, R.E., Catalano, J.G., et al. (2013) A hematite-bearing layer in Gale crater, Mars: Mapping and implications for past aqueous conditions. Geology, 41, 11031106.CrossRefGoogle Scholar
Gaffey, S.J. (1985) Reflectance spectroscopy in the visible and near-infrared (0.35–2.55 µm): Applications in carbonate petrology. Geology, 13, 270273.2.0.CO;2>CrossRefGoogle Scholar
Goldman, D.S. & Rossman, G.R. (1977) The spectra of iron in orthopyroxene revisited: The splitting of the ground state. American Mineralogist, 62, 151157.Google Scholar
Hapke, B. (1981) Bidirectional reflectance spectroscopy, 1. Theory. Journal of Geophysical Research, 86, 30393054.CrossRefGoogle Scholar
Harris, D.C. & Bertolucci, M.D. (1989) Symmetry and spectroscopy: An introduction to vibrational and electronic spectroscopy. Dover Publications, Mineola, NY.Google Scholar
Horgan, B.H.N., Cloutis, E.A., Mann, P., & Bell, J.F. (2014) Near-infrared spectra of ferrous mineral mixtures and methods for their identification in planetary surface spectra. Icarus, 234, 132154.CrossRefGoogle Scholar
Isaacson, P.J., Klima, R.L., Sunshine, J.M., et al. (2014) Visible to near-infrared optical properties of pure synthetic olivine across the olivine solid solution. American Mineralogist, 99, 467478.CrossRefGoogle Scholar
Izenberg, N.R., Klima, R.L., Murchie, S.L., et al. (2014) The low-iron, reduced surface of Mercury as seen in spectral reflectance by MESSENGER. Icarus, 228, 364374.CrossRefGoogle Scholar
Karr, C. (1975) Infrared and Raman spectroscopy of lunar and terrestrial materials. Academic Press, New York.Google Scholar
Klima, R.L., Dyar, M.D., & Pieters, C.M. (2011) Near-infrared spectra of clinopyroxenes: Effects of calcium content and crystal structure. Meteoritics and Planetary Science, 46, 379395.CrossRefGoogle Scholar
Lane, M.D., Bishop, J.L., Dyar, M.D., et al. (2015) Mid-infrared emission spectroscopy and visible/near-infrared reflectance spectroscopy of Fe-sulfate minerals. American Mineralogist, 100, 6682.CrossRefGoogle Scholar
Ling, Z., Cao, F., Ni, Y., Wu, Z., Zhang, J., & Li, B. (2016) Correlated analysis of chemical variations with spectroscopic features of the K–Na jarosite solid solutions relevant to Mars. Icarus, 271, 1929.CrossRefGoogle Scholar
Mao, H.K., Bell, P.M., & Virgo, D. (1977) Crystal-field spectra of fassaite from the Angra dos Reis meteorite. Earth and Planetary Science Letters, 35, 352356.CrossRefGoogle Scholar
Mattson, S.M. & Rossman, G.R. (1988) Fe2+-Ti4+ charge transfer in stoichiometric Fe2+,Ti4+-minerals. Physics and Chemistry of Minerals, 16, 7882.CrossRefGoogle Scholar
McCollom, T.M., Ehlmann, B.L., Wang, A., Hynek, B., Moskowitz, B., & Berquó, T.S. (2014) Detection of iron substitution in natroalunite-natrojarosite solid solutions and potential implications for Mars. American Mineralogist, 99, 948964.CrossRefGoogle Scholar
McCord, T.B., Adams, J.B., & Johnson, T.V. (1970) Asteroid vesta – Spectral reflectivity and compositional implications. Science, 168, 14451447.CrossRefGoogle ScholarPubMed
Meyer, B., Gouterman, M., Jensen, D., Oommen, T.V., Spitzer, K., & Stroyer-Hansen, T. (1972) The spectrum of sulfur and its allotropes. Advances in Chemistry, 110, 5372.CrossRefGoogle Scholar
Morris, R.V., Lauer, H.V. Jr., Lawson, C.A., Gibson, E.K. Jr., Nace, G.A., & Stewart, C. (1985) Spectral and other physicochemical properties of submicron powders of hematite (a-Fe2O3), maghemite (g-Fe2O3), magnetite (Fe3O4), goethite (a-FeOOH), and lepidocrocite (g-FeOOH). Journal of Geophysical Research, 90, 31263144.CrossRefGoogle Scholar
Morris, R.V., Golden, D.C., Bell, J.F. III, et al. (2000) Mineralogy, composition, and alteration of Mars Pathfinder rocks and soils: Evidence from multispectral, elemental, and magnetic data on terrestrial analogue, SNC meteorite, and Pathfinder samples. Journal of Geophysical Research, 105, 17571817.CrossRefGoogle Scholar
Mustard, J.F., Poulet, F., Gendrin, A., et al. (2005) Olivine and pyroxene diversity in the crust of Mars. Science, 307, 15941597.CrossRefGoogle ScholarPubMed
Nash, D.B., Fanale, F.P., & Nelson, R.M. (1980) SO2 Frost: UV‐visible reflectivity and Io surface coverage. Geophysical Research Letters, 7, 665668.CrossRefGoogle Scholar
Pieters, C.M. (1978) Mare basalt types on the front side of the moon – A summary of spectral reflectance data. Proc. 9th Lunar Planet. Sci. Conf., 3, 2825–2849.
Pieters, C.M. (1986) Composition of the lunar highland crust from near-infrared spectroscopy. Reviews of Geophysics, 24, 557578.CrossRefGoogle Scholar
Pieters, C.M., Head, J.W. III, Patterson, W., et al. (1986) The color of Venus. Science, 234, 13791383.CrossRefGoogle ScholarPubMed
Pitman, K.M., Dobrea, E.Z.N., Jamieson, C.S., Dalton, J.B., Abbey, W.J., & Joseph, E.C.S. (2014) Reflectance spectroscopy and optical functions for hydrated Fe-sulfates. American Mineralogist, 99, 15931603.CrossRefGoogle Scholar
Rossman, G.R. (1975) Spectroscopic and magnetic studies of ferric iron hydroxy sulfates: Intensification of color in ferric iron clusters bridged by a single hydroxide ion. American Mineralogist, 60, 698704.Google Scholar
Rossman, G.R. (1976) Spectroscopic and magnetic studies of ferric iron hydroxy sulfates: The series Fe(OH)SO4•nH2O and the jarosites. American Mineralogist, 61, 398404.Google Scholar
Rossman, G.R. (1988) Optical spectroscopy. In: Spectroscopic methods in mineralogy and geology (Hawthorne, F.C., ed.). Mineralogical Society of America, Washington, DC, 207–254.Google Scholar
Rossman, G.R. (1996) Why hematite is red: Correlation of optical absorption intensities and magnetic moments of Fe3+ minerals. In: Mineral spectroscopy: A tribute to Roger G. Burns. Special publication (Geochemical Society). No. 5. Geochemical Society, Houston, TX, 2327.Google Scholar
Rossman, G.R. (2014) Optical spectroscopy. Reviews in Mineralogy and Geochemistry, 78, 371398.CrossRefGoogle Scholar
Sherman, D.M. & Waite, T.D. (1985) Electronic spectra of Fe3+ oxides and oxide hydroxides in the near IR to near UV. American Mineralogist, 70, 12621269.Google Scholar
Sherman, D.M. & Vergo, N. (1988) Optical (diffuse reflectance) and Mössbauer spectroscopic study of nontronite and related Fe-bearing smectites. American Mineralogist, 73, 13461354.Google Scholar
Sklute, E.C., Jensen, H.B., Rogers, A.D., & Reeder, R.J. (2015) Morphological, structural, and spectral characteristics of amorphous iron sulfates. Journal of Geophysical Research, 120, 809830.Google Scholar
Staid, M.I., Pieters, C.M., Besse, S., et al. (2011) The mineralogy of late stage lunar volcanism as observed by the Moon Mineralogy Mapper on Chandrayaan‐1. Journal of Geophysical Research, 116, E00G10, DOI:10.1029/2010JE003735.CrossRefGoogle Scholar
, C.-M., Singer, R.B., Parkin, K.M., & Burns, R.G. (1977) Temperature dependence of Fe2+ crystal field spectra: Implications to mineralogical mapping of planetary surfaces. Proc. 8th Lunar Sci. Conf, 1063–1079.
Sunshine, J.M. & Pieters, C.M. (1993) Estimating modal abundances from the spectra of natural and laboratory pyroxene mixtures using the Modified Gaussian Model. Journal of Geophysical Research, 98, 90759087.CrossRefGoogle Scholar
Sunshine, J.M. & Pieters, C.M. (1998) Determining the composition of olivine from reflectance spectroscopy. Journal of Geophysical Research, 103, 13,675–13,688.CrossRefGoogle Scholar
Vilas, F., Jarvis, K.S., & Gaffey, M.J. (1994) Iron alteration minerals in the visible and near-infrared spectra of low-albedo asteroids. Icarus, 109, 274283.CrossRefGoogle Scholar
Whitten, J. & Head, J.W. (2015) Lunar cryptomaria: Mineralogy and composition of ancient volcanic deposits. Planetary and Space Science, 106, 6781.CrossRefGoogle Scholar
Wildner, M., Andrut, M., & Rudowicz, C.Z. (2004) Optical absorption spectroscopy in geosciences: Part I: Basic concepts of crystal field theory; Part 2: Quantitative aspects of crystal fields. In: Spectroscopic methods in mineralogy (Beran, A. & Libowitzky, E., eds.). Mineralogical Society of Great Britain and Ireland.Google Scholar

References

Arnold, J.A. (2014) Refining mid-infrared emission spectroscopy as a tool for understanding planetary surface mineralogy through laboratory studies, computational models, and lunar remote sensing data. PhD thesis, State University of New York at Stony Brook.
Arnold, J.A., Glotch, T.D., & Plonka, A.M. (2014) Mid-infrared optical constants of clinopyroxene and orthoclase derived from oriented single-crystal reflectance spectra. American Mineralogist, 99, 19421955.CrossRefGoogle Scholar
Aronson, J.R. (1986) Optical constants of monoclinic anisotropic crystals: Orthoclase. Spectrochimica Acta A: Molecular Spectroscopy, 42, 187190.CrossRefGoogle Scholar
Aronson, J.R., Emslie, A.G., Allen, R.V., & McLinden, H.G. (1967) Studies of the middle- and far-infrared spectra of mineral surfaces for application in remote compositional mapping of the Moon and planets. Journal of Geophysical Research, 72, 687703.CrossRefGoogle Scholar
Aronson, J.R., Emslie, A.G., Miseo, E.V., Smith, E.M., & Strong, P.F. (1983) Optical constants of monoclinic anisotropic crystals: Gypsum. Applied Optics, 22, 40934098.CrossRefGoogle ScholarPubMed
Aronson, J.R., Emslie, A.G., & Strong, P.F. (1985) Optical constants of triclinic anisotropic crystals: Blue vitriol. Applied Optics, 24, 12001203.CrossRefGoogle ScholarPubMed
Bandfield, J.L. (2009) Effects of surface roughness and graybody emissivity on martian thermal infrared spectra. Icarus, 202, 414428.CrossRefGoogle Scholar
Bandfield, J.L., Hayne, P.O., Williams, J.-P., Greenhagen, B.T., & Paige, D.A. (2015) Lunar surface roughness derived from LRO Diviner Radiometer observations. Icarus, 248, 357372.CrossRefGoogle Scholar
Belousov, M.V. & Pavinich, V.F. (1978) Infrared reflection spectra of monoclinic crystals. Optics and Spectroscopy, 45, 771774.Google Scholar
Berreman, D.W. (1972) Optics in stratified and anisotropic media: 4×4-matrix formulation. Journal of the Optical Society of America, 62, 502510.CrossRefGoogle Scholar
Bohren, C.F. & Huffman, D.R. (2007) Absorption and scattering of light by small particles. John Wiley & Sons, Hoboken, NJ.Google Scholar
Born, M. & Wolf, E. (1980) Principles of optics. Pergamon Press, Oxford.Google Scholar
Chandrasekhar, S. (1960) Radiative transfer. Dover Publications, Mineola, NY.Google Scholar
Christensen, P.R. & Harrison, S.T. (1993) Thermal infrared emission spectroscopy of natural surfaces: Application to desert varnish coatings on rocks. Journal of Geophysical Research, 98, 19,81919,834.CrossRefGoogle Scholar
Clark, B.E., Bus, S.J., Rivkin, A.S., et al. (2004) E-type asteroid spectroscopy and compositional modeling. Journal of Geophysical Research, 109, E02001, DOI:10.1029/2003JE002200.CrossRefGoogle Scholar
Conel, J.E. (1969) Infrared emissivities of silicates: Experimental results and a cloudy atmosphere model of spectral emission from condensed particulate mediums. Journal of Geophysical Research, 74, 16141634.CrossRefGoogle Scholar
Cooper, C.D. & Mustard, J.F. (2002) Spectroscopy of loose and cemented sulfate-bearing soils: Implications for duricrust on Mars. Icarus, 158, 4255.CrossRefGoogle Scholar
Davidsson, B.J.R., Rickman, H., Bandfield, J.L., et al. (2015) Interpretation of thermal emission. I. The effect of roughness for spatially resolved atmosphereless bodies. Icarus, 252, 121.CrossRefGoogle Scholar
Denevi, B.W., Lucey, P.G., Hochberg, E.J., & Steutel, D. (2007) Near‐infrared optical constants of pyroxene as a function of iron and calcium content. Journal of Geophysical Research, 112, E05009, DOI:10.1029/2006JE002802.CrossRefGoogle Scholar
Donaldson, Hanna K.L., Thomas, I.R., Bowles, N.E., et al. (2012a) Laboratory emissivity measurements of the plagioclase solid solution series under varying environmental conditions. Journal of Geophysical Research, 117, E11004, DOI:10.1029/2012JE004184.Google Scholar
Donaldson, Hanna K.L., Wyatt, M.B., Thomas, I.R., et al. (2012b) Thermal infrared emissivity measurements under a simulated lunar environment: Application to the Diviner Lunar Radiometer experiment. Journal of Geophysical Research, 117, E00H05, DOI:10.1029/2011JE003862.Google Scholar
Donaldson, Hanna K.L., Cheek, L.C., Pieters, C.M., et al. (2014) Global assessment of pure crystalline plagioclase across the Moon and implications for the evolution of the primary crust. Journal of Geophysical Research, 119, 15161545.Google Scholar
Donaldson, Hanna K.L., Greenhagen, B.T., Patterson, W.R., et al. (2017) Effects of varying environmental conditions on emissivity spectra of bulk lunar soils: Application to Diviner thermal infrared observations of the Moon. Icarus, 283, 326342.CrossRefGoogle Scholar
Emslie, A.G. & Aronson, J.R. (1983) Determination of the complex dielectric tensor of triclinic crystals: Theory. Journal of the Optical Society of America, 73, 916919.CrossRefGoogle Scholar
Feely, K.C. & Christensen, P.R. (1999) Quantitative compositional analysis using thermal emission spectroscopy: Application to igneous and metamorphic rocks. Journal of Geophysical Research, 104, 24,19524,210.CrossRefGoogle Scholar
Glotch, T.D. & Rossman, G.R. (2009) Mid-infrared reflectance spectra and optical constants of six iron oxide/oxyhydroxide phases. Icarus, 204, 663671.CrossRefGoogle Scholar
Glotch, T., Rossman, R.G., & Aharonson, O. (2007) Mid-infrared (5–100 μm) reflectance spectra and optical constants of ten phyllosilicate minerals. Icarus, 192, 605622.CrossRefGoogle Scholar
Glotch, T.D., Bandfield, J.L., Tornabene, L.L., Jensen, H.B., & Seelos, F.P. (2010) Distribution and formation of chlorides and phyllosilicates in Terra Sirenum, Mars. Geophysical Research Letters, 37, 15.CrossRefGoogle Scholar
Glotch, T.D., Bandfield, J.L., Lucey, P.G., et al. (2015) Formation of lunar swirls by magnetic field standoff of the solar wind. Nature Communications, 6, 6189.CrossRefGoogle ScholarPubMed
Glotch, T.D., Bandfield, J.L., Wolff, M.J., Arnold, J.A., & Che, C. (2016) Constraints on the composition and particle size of chloride salt-bearing deposits on Mars. Journal of Geophysical Research, 121, 454471.Google Scholar
Greenhagen, B.T., Lucey, P.G., Wyatt, M.B., et al. (2010) Global silicate mineralogy of the Moon from the Diviner Lunar Radiometer. Science, 329, 1507.CrossRefGoogle ScholarPubMed
Hapke, B. (1981) Bidirectional reflectance spectroscopy, 1. Theory. Journal of Geophysical Research, 86, 30393054.CrossRefGoogle Scholar
Hapke, B. (1993/2012) Theory of reflectance and emittance spectroscopy. Cambridge University Press, Cambridge.CrossRefGoogle Scholar
Hapke, B. (1996) A model of radiative and conductive energy transfer in planetary regoliths. Journal of Geophysical Research, 101, 1681716831.CrossRefGoogle Scholar
Hardgrove, C.J., Rogers, A.D., Glotch, T.D., & Arnold, J.A. (2016) Thermal emission spectroscopy of microcrystalline sedimentary phases: Effects of natural surface roughness on spectral feature shape. Journal of Geophysical Research, 121, 542555.Google Scholar
Henderson, B.G. & Jakosky, B.M. (1994) Near-surface thermal gradients and their effects on mid-infrared emission spectra of planetary surfaces. Journal of Geophysical Research, 99, 1906319073.CrossRefGoogle Scholar
Henderson, B.G. & Jakosky, B.M. (1997) Near‐surface thermal gradients and mid‐IR emission spectra: A new model including scattering and application to real data. Journal of Geophysical Research, 102, 65676580.CrossRefGoogle Scholar
Henderson, B.G., Lucey, P.G., & Jakosky, B.M. (1996) New laboratory measurements of mid‐IR emission spectra of simulated planetary surfaces. Journal of Geophysical Research, 101, 1496914975.CrossRefGoogle Scholar
Hiroi, T. (1994) Recalculation of the isotropic H-functions. Icarus, 109(2), 313317.CrossRefGoogle Scholar
Höfer, S., Werling, S., & Beyerer, J. (2013) Thermal pattern generation for infrared deflectometry. AMA Conferences 2013 – Nürnberg Exhibition Centre, May 14–16, 2013 – SENSOR, OPTO and IRS², 785790.
Huffman, D.R. & Stapp, J.L. (1971) Interstellar silicate extinction related to the 2200 Å band. Nature Physical Science, 229, 45.CrossRefGoogle Scholar
Ito, G., Arnold, J.A., & Glotch, T.D. (2017) T‐matrix and radiative transfer hybrid models for densely packed particulates at mid‐infrared wavelengths. Journal of Geophysical Research, 122, 822838.Google Scholar
Keshava, N. & Mustard, J.F. (2002) Spectral unmixing. IEEE Signal Processing Magazine, 19(1), 4457, DOI:10.1109/79.974727.CrossRefGoogle Scholar
Lane, M.D. (1999) Midinfrared optical constants of calcite and their relationship to particle size effects in thermal emission spectra of granular calcite. Journal of Geophysical Research, 104, 1409914108.CrossRefGoogle Scholar
Lawrence, S.J. & Lucey, P.G. (2007) Radiative transfer mixing models of meteoritic assemblages. Journal of Geophysical Research, 112, E07005, DOI:10.1029/2006JE002765.CrossRefGoogle Scholar
Li, S. & Li, L. (2011) Radiative transfer modeling for quantifying lunar surface minerals, particle size, and submicroscopic metallic Fe. Journal of Geophysical Research, 116, E09001, DOI:10.1029/2011JE003837.CrossRefGoogle Scholar
Li, S. & Milliken, R.E. (2015) Estimating the modal mineralogy of eucrite and diogenite meteorites using visible–near infrared reflectance spectroscopy. Meteoritics and Planetary Science, 50, 18211850.CrossRefGoogle Scholar
Liu, Y., Glotch Timothy, D., Scudder Noel, A., et al. (2016) End‐member identification and spectral mixture analysis of CRISM hyperspectral data: A case study on southwest Melas Chasma, Mars. Journal of Geophysical Research, 121, 20042036.Google Scholar
Logan, L.M. & Hunt, G.R. (1970) Emission spectra of particulate silicates under simulated lunar conditions. Journal of Geophysical Research, 75, 65396548.CrossRefGoogle Scholar
Logan, L.M., Hunt, G.R., Salisbury, J.W., & Balsamo, S.R. (1973) Compositional implications of Christiansen frequency maximums for infrared remote sensing applications. Journal of Geophysical Research, 78, 49835003.CrossRefGoogle Scholar
Long, L.L., Querry, M.R., Bell, R.J., & Alexander, R.W. (1993) Optical properties of calcite and gypsum in crystalline and powdered form in the infrared and far-infrared. Infrared Physics, 34, 191201.CrossRefGoogle Scholar
Lucey, P.G. (1998) Model near-infrared optical constants of olivine and pyroxene as a function of iron content. Journal of Geophysical Research, 103, 17031713.CrossRefGoogle Scholar
Mackowski, D.W. (1994) Calculation of total cross sections of multiple-sphere clusters. Journal of the Optical Society of America A, 11, 28512861.CrossRefGoogle Scholar
Mackowski, D.W. & Mishchenko, M.I. (1996) Calculation of the T matrix and the scattering matrix for ensembles of spheres. Journal of the Optical Society of America A, 13, 22662278.CrossRefGoogle Scholar
Mackowski, D.W. & Mishchenko, M.I. (2011) A multiple sphere T-matrix Fortran code for use on parallel computer clusters. Journal of Quantitative Spectroscopy and Radiative Transfer, 112, 21822192.CrossRefGoogle Scholar
Mayerhöfer, T. & Popp, J. (2007) Employing spectra of polycrystalline materials for the verification of optical constants obtained from corresponding low-symmetry single crystals. Applied Optics, 46, 327334.CrossRefGoogle Scholar
Mie, G. (1908) Beiträge zur Optik trüber Medien, speziell kolloidaler Metallösungen. Annalen der Physik, 330, 377445.CrossRefGoogle Scholar
Millán, L., Thomas, I., & Bowles, N. (2011) Lunar regolith thermal gradients and emission spectra: Modeling and validation. Journal of Geophysical Research, 116, DOI: 10.1029/2011JE003874.CrossRefGoogle Scholar
Mishchenko, M.I. (1994) Asymmetry parameters of the phase function for densely packed scattering grains. Journal of Quantitative Spectroscopy and Radiative Transfer, 52, 95110.CrossRefGoogle Scholar
Moersch, J.E. & Christensen, P.R. (1995) Thermal emission from particulate surfaces: A comparison of scattering models with measured spectra. Journal of Geophysical Research, 100, 74657477.CrossRefGoogle Scholar
Murcray, F.H., Murcray, D.G., & Williams, W.J. (1970) Infrared emissivity of lunar surface features: 1. Balloon‐borne observations. Journal of Geophysical Research, 75, 26622669.CrossRefGoogle Scholar
Mustard, J.F. & Pieters, C.M. (1987) Quantitative abundance estimates from bidirectional reflectance measurements. Journal of Geophysical Research, 92, E617E626.CrossRefGoogle Scholar
Mustard, J.F. & Pieters, C.M. (1989) Photometric phase functions of common geologic minerals and applications to quantitative analysis of mineral mixture reflectance spectra. Journal of Geophysical Research, 94, 1361913634.CrossRefGoogle Scholar
Mustard, J.F. & Hays, J.E. (1997) Effects of hyperfine particles on reflectance spectra from 0.3 to 25 µm. Icarus, 125, 145163.CrossRefGoogle Scholar
Mustard, J.F. & Sunshine, J.M. (1999) Spectral analysis for Earth science: Investigations using remote sensing data. Remote sensing for the Earth sciences: Manual of remote sensing, 3 (Rencz, A., ed.). John Wiley & Sons, New York, 251307.Google Scholar
Mustard, J.F., Li, L., & He, G.Q. (1998) Nonlinear spectral mixture modeling of lunar multispectral data: Implications for lateral transport. Journal of Geophysical Research, 103, 1941919425.CrossRefGoogle Scholar
Osterloo, M.M., Hamilton, V.E., Bandfield, J.L., et al. (2008) Chloride-bearing materials in the southern highlands of Mars. Science, 319, 16511654.CrossRefGoogle ScholarPubMed
Osterloo, M.M., Anderson, F.S., Hamilton, V.E., & Hynek, B.M. (2010) Geologic context of proposed chloride-bearing materials on Mars. Journal of Geophysical Research, 115, E10012, DOI:10.1029/2010JE003613.CrossRefGoogle Scholar
Pitman, K.M., Wolff, M.J., & Clayton, C. (2005) Application of modern radiative transfer tools to model laboratory quartz emissivity. Journal of Geophysical Research, 110, E08003, DOI:10.1029/2005JE002428.CrossRefGoogle Scholar
Poulet, F. & Erard, S. (2004) Nonlinear spectral mixing: Quantitative analysis of laboratory mineral mixtures. Journal of Geophysical Research, 109, DOI:10.1029/2003JE002179.CrossRefGoogle Scholar
Poulet, F., Bibring, J.P., Langevin, Y., et al. (2009) Quantitative compositional analysis of martian mafic regions using the MEx/OMEGA reflectance data. Icarus, 201(1), 6983, DOI:10.1016/J.Icarus.2008.12.025.CrossRefGoogle Scholar
Ramsey, M.S. & Christensen, P.R. (1998) Mineral abundance determination: Quantitative deconvolution of thermal emission spectra. Journal of Geophysical Research, 103, 577596.CrossRefGoogle Scholar
Robertson, K.M., Milliken, R.E., & Li, S. (2016) Estimating mineral abundances of clay and gypsum mixtures using radiative transfer models applied to visible-near infrared reflectance spectra. Icarus, 277, 171186.CrossRefGoogle Scholar
Rogers, A.D. & Aharonson, O. (2008) Mineralogical composition of sands in Meridiani Planum determined from Mars Exploration Rover data and comparison to orbital measurements. Journal of Geophysical Research, 113, E06S14, DOI:10.1029/2007JE002995.CrossRefGoogle Scholar
Roush, T.L., Pollack, J.B., & Orenberg, J. (1991) Derivation of midinfrared (5–25 µm) optical constants of some silicates and palagonite. Icarus, 94, 191208.CrossRefGoogle Scholar
Roush, T., Esposito, F., Rossman, G.R., & Colangeli, L. (2007) Estimated optical constants of gypsum in the regions of weak absorptions: Application of scattering theories and comparisons to independent measurements. Journal of Geophysical Research, 112, DOI:10.1029/2007JE002920.CrossRefGoogle Scholar
Salisbury, J.W. & Wald, A. (1992) The role of volume scattering in reducing spectral contrast of reststrahlen bands in spectra of powdered minerals. Icarus, 96, 121128.CrossRefGoogle Scholar
Salisbury, J.W. & Walter, L.S. (1989) Thermal infrared (2.5–13.5 µm) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces. Journal of Geophysical Research, 94, 91929202.CrossRefGoogle Scholar
Salisbury, F.B., Wald, A., & D’Aria, D.M. (1994) Thermal-infrared remote sensing and Kirchhoff’s law 1. Laboratory measurements. Journal of Geophysical Research, 99, 1189711911.CrossRefGoogle Scholar
Shirley, K.A. & Glotch, T.D. (2019) Particle size effects on mid-IR spectra of lunar analog materials in a simulated lunar environment. Journal of Geophysical Research, 124, 970–988.
Shirley, K.A., Glotch, T.D., Greenhagen, B.T., & White, M. (2015) A multiplicative approach to correcting the thermal channels for the Diviner Lunar Radiometer Experiment. 46th Lunar Planet. Sci. Conf., Abstract #1992.
Shkuratov, Y., Starukhina, L., Hoffmann, H., & Arnold, G. (1999) A model of spectral albedo of particulate surfaces: Implications for optical properties of the Moon. Icarus, 137, 235246.CrossRefGoogle Scholar
Sklute, E.C., Glotch, T.D., Piatek, J., Woerner, W., Martone, A., & Kraner, M. (2015) Optical constants of synthetic potassium, sodium, and hydronium jarosite. American Mineralogist, 100, 11101122.CrossRefGoogle Scholar
Spitzer, W.G. & Kleinman, D.A. (1961) Infrared lattice bands of quartz. Physical Review, 121, 13241335.CrossRefGoogle Scholar
Stamnes, K., Tsay, S.-C., Wiscombe, W., & Jayaweera, K. (1988) Numerically stable algorithm for discrete-ordinate-method radiative transfer in multiple scattering and emitting layered media. Applied Optics, 27, 25022509.CrossRefGoogle ScholarPubMed
Swanepoel, R. (1983) Determination of the thickness and optical constants of amorphous silicon. Journal of Physics E: Scientific Instruments, 16, 1214.CrossRefGoogle Scholar
Thomas, I.R., Greenhagen, B.T., Bowles, N.E., Donaldson Hanna, K.L., Temple, J., & Calcutt, S.B. (2012) A new experimental setup for making thermal emission measurements in a simulated lunar environment. Review of Scientific Instruments, 83, 124502.CrossRefGoogle Scholar
Trang, D., Lucey Paul, G., Gillis‐Davis Jeffrey, J., Cahill Joshua, T.S., Klima Rachel, L., & Isaacson Peter, J. (2013) Near‐infrared optical constants of naturally occurring olivine and synthetic pyroxene as a function of mineral composition. Journal of Geophysical Research, 118, 708732.Google Scholar
Van de Hulst, H.C. (1957) Light scattering by small particles. Dover Publications, Mineola, NY.CrossRefGoogle Scholar
Wald, A.E. (1994) Modeling thermal infrared (2–14 μm) reflectance spectra of frost and snow. Journal of Geophysical Research, 99, 24,24124,250.CrossRefGoogle Scholar
Wald, A.E. & Salisbury, J.W. (1995) Thermal infrared directional emissivity of powdered quartz. Journal of Geophysical Research, 100, 2466524675.CrossRefGoogle Scholar
Wenrich, M.L. & Christensen, P.R. (1996) Optical constants of minerals derived from emission spectroscopy: Application to quartz. Journal of Geophysical Research, 101, 1592115931.CrossRefGoogle Scholar

References

Adler, H.H. & Kerr, P.F. (1963) Infrared spectra, symmetry and structure relations of some carbonate minerals. American Mineralogist, 48, 839853.Google Scholar
Adler, H.H. & Kerr, P.F. (1965) Variations in infrared spectra, molecular symmetry and site symmetry of sulfate minerals. American Mineralogist, 50, 132147.Google Scholar
Arnold, J.A., Glotch, T.D., & Plonka, A.M. (2014) Mid-infrared optical constants of clinopyroxene and orthoclase derived from oriented single-crystal reflectance spectra. American Mineralogist, 99, 19421955.CrossRefGoogle Scholar
Aronson, J.R. & Elmslie, A.G. (1973) Spectral reflectance and emittance of particulate materials. 2: Application and results. Applied Optics, 12, 25732585.CrossRefGoogle ScholarPubMed
Aronson, J.R., Emslie, A.G., & McLinden, H.G. (1966) Infrared spectra from particulate surfaces. Science, 152, 345346.CrossRefGoogle ScholarPubMed
Ashley, J.W. (2011) Meteorites on Mars as Planetary Research Tools with Special Considerations for Martian Weathering Processes. PhD dissertation, Arizona State University.
Ashley, J.W. & Christensen, P.R. (2012) Thermal emission spectroscopy of unpowdered meteorites. 43rd Lunar Planet. Sci. Conf., Abstract #2519.
Baldridge, A.M. & Christensen, P.R. (2009) A laboratory technique for thermal emission measurement of hydrated minerals. Applied Spectroscopy, 63, 678688.CrossRefGoogle ScholarPubMed
Baldridge, A.M., Hook, S.J., Grove, C.I., & Rivera, G. (2009) The ASTER spectral library version 2.0. Remote Sensing of the Environment, 13, 711715.CrossRefGoogle Scholar
Bishop, J.L., Lane, M.D., Dyar, M.D., & Brown, A.J. (2008) Reflectance and emission spectroscopy study of four groups of phyllosilicates: Smectites, kaolinite-serpentines, chlorites and micas. Clay Minerals, 43, 3554.CrossRefGoogle Scholar
Bishop, J.L., Lane, M.D., Dyar, M.D., King, S.J., Brown, A.J., & Swayze, G. (2014a) Spectral properties of Ca-sulfates: Gypsum, bassanite, and anhydrite. American Mineralogist, 99, 21052115.CrossRefGoogle Scholar
Bishop, J.L., Quinn, R., & Dyar, M.D. (2014b) Spectral and thermal properties of perchlorate salts and implications for Mars. American Mineralogist, 99, 15801592.CrossRefGoogle Scholar
Bishop, J.L., Murad, E., & Dyar, M.D. (2015) Akaganéite and schwertmannite: Spectral properties, structural models and geochemical implications of their possible presence on Mars. American Mineralogist, 100, 738746.CrossRefGoogle Scholar
Bishop, J.L., King, S.J., Lane, M.D., et al. (2017) Spectral properties of anhydrous carbonates and nitrates. 48th Lunar Planet. Sci. Conf., Abstract #2362.
Born, M. & Wolf, E. (1980) Principles of Optics, 6th edn. Pergamon, Tarrytown, NY, 627633.Google Scholar
Böttcher, M.E., Gehlken, P.-L., Fernandez-Gonzalez, A., & Prieto, M. (1997) Characterization of synthetic BaCO3–SrCO3 (witherite-strontianite) solid-solutions by Fourier transform infrared spectroscopy. European Journal of Mineralogy, 9, 519528.CrossRefGoogle Scholar
Che, C. & Glotch, T.D. (2012) The effect of high temperatures on the mid-to-far-infrared and near-infrared reflectance spectra of phyllosilicates and natural zeolites: Implications for martian exploration. Icarus, 218, 585601.CrossRefGoogle Scholar
Che, C., Glotch, T.D., Bish, D.L., Michalski, J.R., & Xu, W. (2011) Spectroscopic study of the dehydration and/or dehydroxylation of phyllosilicate and zeolite minerals. Journal of Geophysical Research, 116, DOI:10.1029/2010JE003740.CrossRefGoogle Scholar
Chen, Y., Zou, C., Mastalerz, M., Hu, S., Gasaway, C., & Tao, X. (2015) Applications of micro-Fourier Transform Infrared Spectroscopy (FTIR) in the geological sciences: A review. International Journal of Molecular Sciences, 16, 26227.CrossRefGoogle ScholarPubMed
Chihara, H., Koike, C., Tsuchiyama, A., Tachibana, S., & Sakamoto, D. (2002) Compositional dependence of infrared absorption spectra of crystalline silicates. I. Mg-Fe pyroxenes. Astronomy & Astrophysics, 391, 267273.CrossRefGoogle Scholar
Christensen, P.R. & Harrison, S.T. (1993) Thermal infrared emission spectroscopy of natural surfaces: Application to desert varnish coatings on rocks. Journal of Geophysical Research, 98, 19,81919,834.CrossRefGoogle Scholar
Christensen, P.R., Bandfield, J.L., Hamilton, V.E., et al. (2000a) A thermal emission spectral library of rock-forming minerals. Journal of Geophysical Research, 105, 97359739.CrossRefGoogle Scholar
Christensen, P.R., Bandfield, J.L., Clark, R.N., et al. (2000b) Detection of crystalline hematite mineralization on Mars by the Thermal Emission Spectrometer: Evidence for near-surface water. Journal of Geophysical Research, 105, 96239642.CrossRefGoogle Scholar
Christensen, P.R., Morris, R.V., Lane, M.D., Bandfield, J.L., & Malin, M.C. (2001) Global mapping of martian hematite mineral deposits: Remnants of water-driven processes on early Mars. Journal of Geophysical Research, 106, 2387323885.CrossRefGoogle Scholar
Clark, R.N., Swayze, G.A., Wise, R., et al. (2007) USGS Digital Spectral Library splib06a: U.S. Geological Survey, Digital Data Series 231.CrossRef
Cloutis, E.A. (2015) The University of Winnepeg’s Planetary Spectrophotometer Facility (aka HOSERLab): What’s new. 46th Lunar Planet. Sci. Conf., Abstract #1187.
Cloutis, E.A., Pranoti, M.A., & Mertzman, S.A. (2002) Spectral reflectance properties of zeolites and remote sensing implications. Journal of Geophysical Research, 107, E9, DOI:1029/2000JE001467.CrossRefGoogle Scholar
Coblentz, W.W. (1905) Investigations of infra-red spectra, 35. Carnegie Institution Publications, Washington, DC.Google Scholar
Coblentz, W.W. (1906) Investigations of infra-red spectra, 65. Carnegie Institution Publications, Washington, DC.Google Scholar
Coblentz, W.W. (1908) Investigations of infra-red spectra, 97. Carnegie Institution Publications, Washington, DC.Google Scholar
Conel, J.E. (1965) Infrared thermal emission from silicates. Jet Propulsion Laboratory Technical Memorandum 33–243.
Conel, J.E. (1969) Infrared emissivities of silicates: Experimental results and a cloudy atmosphere model of spectral emission from condensed particulate mediums. Journal of Geophysical Research, 74, 16141634.CrossRefGoogle Scholar
Cooper, C.D. & Mustard, J.F. (1999) Effects of very fine particle size on reflectance spectra of smectite and palagonitic soil. Icarus, 142, 557570.CrossRefGoogle Scholar
Cooper, B.L., Salisbury, J.W., Killen, R.M., & Potter, A.E. (2002), Midinfrared spectral features of rocks and their powders. Journal of Geophysical Research, 107, 5017, 10.1029/2001JE001462.CrossRefGoogle Scholar
Crowley, J.K. & Hook, S.J. (1996) Mapping playa evaporate minerals and associated sediments in Death Valley, California, with multispectral thermal infrared images. Journal of Geophysical Research, 101, 643660.CrossRefGoogle Scholar
Dominguez, G., McLeod, A.S., Gainsforth, Z., et al. (2014) Nanoscale infrared spectroscopy as a non-destructive probe of extraterrestrial samples. Nature Communications, 5, 5445.CrossRefGoogle Scholar
Donaldson Hanna, K. & Sprague, A.L. (2009) Vesta and the HED meteorites: Mid-infrared modeling of minerals and their abundances. Meteoritics and Planetary Science, 44(11), 17551770.CrossRefGoogle Scholar
Donaldson Hanna, K.L., Thomas, I.R., Bowles, N.E., et al. (2012) Laboratory emissivity measurements of the plagioclase solid solution series under varying environmental conditions. Journal of Geophysical Research, 117, E11004, DOI:10.1029/2012JE004184.CrossRefGoogle Scholar
Donaldson Hanna, K.L., Greenhagen, B.T., Patterson, W.R. III, et al. (2017) Effects of varying environmental conditions on emissivity spectra of bulk lunar soils: Application to Diviner thermal infrared observations of the Moon. Icarus, 283, 326–342.CrossRef
Dyar, M.D., Glotch, T.D., Lane, M.D., et al. (2011) Spectroscopy of Yamato 984028. Polar Science, 4, 530549.CrossRefGoogle Scholar
Edwards, C.S. & Christensen, P.R. (2013) Microscopic emission and reflectance thermal infrared spectroscopy: Instrumentation for quantitative in situ mineralogy of complex planetary surfaces, Applied Optics, 52, 22002217.CrossRefGoogle ScholarPubMed
Estep-Barnes, P.A. (1977) Infrared spectroscopy. In Zussman, J. (ed.), Physical methods in determinative mineralogy, 2nd edn. Academic Press, New York, 529603.Google Scholar
Farmer, V.C. (1974) The infrared spectra of minerals. The Mineralogical Society, London.CrossRefGoogle Scholar
Feely, K.C. & Christensen, P.R. (1999) Quantitative compositional analysis using thermal emission spectroscopy: Application to igneous and metamorphic rocks. Journal of Geophysical Research, 104, 24,19524,210.CrossRefGoogle Scholar
Friedlander, L.R., Glotch, T.D., Bish, D.L., et al. (2015) Structural and spectroscopic changes to natural nontronite induced by experimental impacts between 10 and 40 GPa. Journal of Geophysical Research, 120, 888912.Google Scholar
Frost, R.L., Kloprogge, T., Martens, W.N., & Williams, P. (2002) Vibrational spectroscopy of the basic manganese, ferric and ferrous phosphate minerals: Strunzite, ferristrunzite, and ferrostrunzite. Neues Jahrbuch für Mineralogie, Monatshefte, 11, 481496.CrossRefGoogle Scholar
Gadsden, J.A. (1975) Infrared spectra of minerals and related inorganic compounds. Butterworth & Co, London.Google Scholar
Glotch, T.D. & Rossman, G.R. (2009) Mid-infrared reflectance spectra and optical constants of six oxide/oxyhydroxide phases. Icarus, 204, 663671.CrossRefGoogle Scholar
Glotch, T.D., Christensen, P.R., & Sharp, T.G. (2006) Fresnel modeling of hematite crystal surfaces and application to martian hematite spherules. Icarus, 181, 408418.CrossRefGoogle Scholar
Glotch, T.D., Rossman, G.R., & Aharonson, O. (2007) Mid-infrared (5–100 μm) reflectance spectra and optical constants of ten phyllosilicate minerals. Icarus, 192, 605622.CrossRefGoogle Scholar
Goodrich, C.A., Kita, N.T., Yin, Q., et al. (2017) Petrogenesis and provenance of ungrouped achondrite Northwest Africa 7325 from petrology, trace elements, oxygen, chromium and titanium isotopes, and mid-IR spectroscopy. Geochimica et Cosmochimica Acta, 203, 381403.CrossRefGoogle ScholarPubMed
Hamilton, V.E. (2000) Thermal infrared emission spectroscopy of the pyroxene mineral series. Journal of Geophysical Research, 105, 97019716.CrossRefGoogle Scholar
Hamilton, V.E. (2010) Thermal infrared (vibrational) spectroscopy of Mg-Fe olivines: A review and applications to determining the composition of planetary surfaces. Chemie der Erde, 70, 733.CrossRefGoogle Scholar
Hamilton, V.E. & Christensen, P.R. (2000) Determining the modal mineralogy of mafic and ultramafic igneous rocks using thermal emission spectroscopy. Journal of Geophysical Research, 105, 97179733.CrossRefGoogle Scholar
Hamilton, V.E., Wyatt, M.B., McSween, H.Y. Jr., & Christensen, P.R. (2001) Analysis of terrestrial and martian volcanic compositions using thermal emission spectroscopy. 2. Application to martian surface spectra from the Mars Global Surveyor Thermal Emission Spectrometer. Journal of Geophysical Research, 106(7), 1472214746.CrossRefGoogle Scholar
Hamilton, V.E., Christensen, P.R., McSween, H.Y. Jr., & Bandfield, J.L. (2003) Searching for the source regions of Martian meteorites using MGS TES: Integrating martian meteorites into the global distribution of igneous materials on Mars. Meteoritics and Planetary Science, 38(6), 871885.CrossRefGoogle Scholar
Hapke, B. (1993) Theory of reflectance and emittance spectroscopy. Cambridge University Press, Cambridge.CrossRefGoogle Scholar
Helbert, J., Moroz, L.V., Maturilli, A., et al. (2007) A set of laboratory analogue materials for the MERTIS instrument on the ESA BepiColombo mission to Mercury. Advanced Space Research, 40, 272279.CrossRefGoogle Scholar
Hellwege, K.H., Lesch, W., Plihal, M., & Schaack, G. (1970) Zwei-Phononen-Absorptionsspektren und Dispersion der Schwingungszweige in Kristallen der Kalkspatstruktur. Zeitschrift für Physik, 232, 6186.CrossRefGoogle Scholar
Henderson, B.G. & Jakosky, B.M. (1997) Near-surface thermal gradients and mid-IR emission spectra: A new model including scattering and application to real data. Journal of Geophysical Research, 102, 65676580.CrossRefGoogle Scholar
Huminicki, D.M.C. & Hawthorne, F.C. (2002) The crystal chemistry of the phosphate minerals. In: Phosphates: Geochemical, geobiological, and materials importance (Kohn, M.J., Rakovan, J., & Hughes, J.M., eds.). Reviews in Mineralogy and Geochemistry. Mineralogical Society of America, Washington, DC, 48, 123253.CrossRefGoogle Scholar
Hunt, G.R. & Vincent, R.K. (1968) The behavior of spectral features in the infrared emission from particulate surfaces of various grain sizes. Journal of Geophysical Research, 73, 60396046.CrossRefGoogle Scholar
Johnson, J.R., Hörz, F. & Staid, M.I. (2003) Thermal infrared spectroscopy and modeling of experimentally shocked plagioclase feldspars. American Mineralogist, 88, 15751582.CrossRefGoogle Scholar
Keller, L.P., Bajt, S., Baratta, G.A., et al. (2006) Infrared spectroscopy of comet 81P/Wild 2 samples returned by Stardust. Science, 314, 17281731.CrossRefGoogle ScholarPubMed
Kereszturi, A., Gyollai, I., & Szabó, M. (2015) Case study of chondrule alteration with IR spectroscopy in NWA 2086 CV3 meteorite. Planetary and Space Science, 106, 122131.CrossRefGoogle Scholar
King, P.L., Ramsey, M.S., McMillan, P.F., & Swayze, G.A. (2004) Laboratory Fourier Transform Infrared Spectroscopy methods for geologic samples. In: Infrared Spectroscopy in Geochemistry, Exploration Geochemistry and Remote Sensing (King, P.L., Ramsey, M.S., & Swayze, G.A., eds.). Mineralogical Association of Canada, Short Course 33, 57–91.Google Scholar
Klima, R.L. & Pieters, C.M. (2006) Near- and mid-infrared microspectroscopy of the Ronda peridotite. Journal of Geophysical Research, 111, DOI:10.1029/2005JE002537.CrossRefGoogle Scholar
Kodama, H. (1985) Infrared Spectra of Minerals: Reference Guide to Identification and Characterization of Minerals for The Study of Soils. Agriculture Canada, Ottawa.Google Scholar
Koike, C., Chihara, H., Tsuchiyama, A., Suto, H., Sogawa, H., & Okuda, H. (2003) Compositional dependence of infrared absorption spectra of crystalline silicate. II. Natural and synthetic olivines. Astronomy & Astrophysics, 399, 11011107.CrossRefGoogle Scholar
Kokaly, R.F., Clark, R.N., Swayze, G.A., et al. (2017) USGS Spectral Library Version 7, USGS Data Series, Reston, VA.CrossRef
Lane, M.D. (1999) Midinfrared optical constants of calcite and their relationship to particle size effects in thermal emission spectra of granular calcite. Journal of Geophysical Research, 104, 1409914108.CrossRefGoogle Scholar
Lane, M.D. (2007) Midinfrared emission spectroscopy of sulfate and sulfate-bearing minerals. American Mineralogist, 92, 118.CrossRefGoogle Scholar
Lane, M.D. & Christensen, P.R. (1997) Thermal infrared emission spectroscopy of anhydrous carbonates. Journal of Geophysical Research, 102, 2558125592.CrossRefGoogle Scholar
Lane, M.D. & Christensen, P.R. (1998) Thermal infrared emission spectroscopy of salt minerals predicted for Mars. Icarus, 135, 528536.CrossRefGoogle Scholar
Lane, M.D., Morris, R.V., Mertzman, S.A., & Christensen, P.R. (2002) Evidence for platy hematite grains in Sinus Meridiani, Mars. Journal of Geophysical Research, 107(E12), 5126, DOI:10.1029/2001JE001832.CrossRefGoogle Scholar
Lane, M.D., Glotch, T.D., Dyar, M.D., et al. (2011a) Midinfrared spectroscopy of synthetic olivines: Thermal emission, specular and diffuse reflectance, and attenuated total reflectance studies of forsterite to fayalite. Journal of Geophysical Research, 116, E08010, DOI:10.1029/2010JE003588.CrossRefGoogle Scholar
Lane, M.D., Mertzman, S.A., Dyar, M.D., & Bishop, J.L. (2011b) Phosphate minerals measured in the visible-near infrared and thermal infrared: Spectra and XRD analyses. 42nd Lunar Planet. Sci. Conf., Abstract #1013.
Lane, M.D., Bishop, J.L., Dyar, M.D., et al. (2015) Mid-infrared emission spectroscopy and visible/near-infrared reflectance spectroscopy of Fe-sulfate minerals. American Mineralogist, 100, 6682, DOI:10.2138/am-2015-4762.CrossRefGoogle Scholar
Logan, L.M. & Hunt, G.R. (1970) Emission spectra of particulate silicates under simulated lunar conditions. Journal of Geophysical Research, 75, 65396548.CrossRefGoogle Scholar
Logan, L.M., Hunt, G.R., Salisbury, J.W., & Balsamo, S.R. (1973) Compositional implications of Christiansen frequency maximums for infrared remote sensing applications. Journal of Geophysical Research, 78, 49835003.CrossRefGoogle Scholar
Long, L.L., Querry, M.R., Bell, R.J., & Alexander, R.W. (1993) Optical properties of calcite and gypsum in crystalline and powdered form in the infrared and far-infrared. Infrared Physics, 34, 191201.CrossRefGoogle Scholar
Lorentz, H.A. (1880) Über die Beziehung zwischen der Fortpflanzungsgeschwindigkeit des Lichtes und der Körperdichte. Annalen der Physik, 245, 641665.CrossRefGoogle Scholar
Lorenz, L. (1881) Über die Refractionsconstante. Annalen der Physik, 247, 70103.CrossRefGoogle Scholar
Lyon, R.J.P. (1964) Evaluation of infrared spectrophotometry for compositional analysis of lunar and planetary soils. II. Rough and powdered surfaces. NASA Contract Report, CR-100.
Lyon, R.J.P. (1965) Analysis of rocks by spectral infrared emission (8–25 µm). Economic Geology, 60, 715736.CrossRefGoogle Scholar
Lyon, R.J.P. & Burns, E.A. (1963) Analysis of rocks and minerals by reflected infrared radiation. Economic Geology, 58, 274284.CrossRefGoogle Scholar
Marino, M., Carati, A., & Galgani, L. (2007) Classical light dispersion theory in a regular lattice. Annals of Physics, 322, 799823.CrossRefGoogle Scholar
Maturilli, A., Helbert, J., Witzke, A., & Moroz, L. (2006) Emissivity measurements of analogue materials for the interpretation of data from PFS on Mars Express and MERTIS on Bepi-Colombo. Planetary and Space Science, 54(11), 10571064.CrossRefGoogle Scholar
Maturilli, A., Helbert, J., & Moroz, L. (2008) The Berlin emissivity database (BED). Planetary and Space Science, 56(3–4), 420425. Spectral library now available at figshare.com/articles/BED_Emissivity_Spectral_Library/1536469.CrossRefGoogle Scholar
Maturilli, A., Helbert, J., Ferrari, S., Davidsson, B., & D’Amore, M. (2016) Characterization of asteroid analogues by means of emission and reflectance spectroscopy in the 1- to 100-m spectral range. Earth Planets and Space, 68(1), article ID 113, 111.CrossRefGoogle Scholar
Michalski, J.R., Kraft, M.D., Diedrich, T., Sharp, T.G., & Christensen, P.R. (2003) Thermal emission spectroscopy of the silica polymorphs and considerations for remote sensing of Mars. Geophysical Research Letters, 30, DOI:10.1029/2003GL018354.CrossRefGoogle Scholar
Michalski, J.R., Kraft, M.D., Sharp, T.G., Williams, L.B., & Christensen, P.R. (2006) Emission spectroscopy of clay minerals and evidence for poorly crystalline aluminosilicates on Mars from Thermal Emission Spectrometer data. Journal of Geophysical Research, 111 (E3), DOI:10.1029/2005JE002438.CrossRefGoogle Scholar
Milam, K.A., McSween, H.Y. Jr., & Christensen, P.R. (2007) Plagioclase compositions derived from thermal emission spectra of compositionally complex mixtures: Implications for martian feldspar mineralogy. Journal of Geophysical Research, 112, DOI:10.1029/2006JE002880.CrossRefGoogle Scholar
Milosevic, M. (2012) Internal Reflection and ATR Spectroscopy. In: Chemical analysis: A series of monographs on analytical chemistry and its applications (Mark F. Vitha, Series Editor). John Wiley & Sons, New York.CrossRefGoogle Scholar
Moenke, H. (1962) Mineralspektren I: Die Ultrarotabsorption der Häufigsten und Wirtschaftlich Wichtigsten Halogenid-, Oxyd-, Hydroxyd-, Carbonat-, Nitrat-, Borat-, Sulfat-, Chromat-, Wolframat-, Molybdat-, Phosphat-, Arsenat-, Vanadat- und Silikatmineralien im Spektralbereich 400–4000 cm–1. Akademie Verlag, Berlin.Google Scholar
Moenke, H. (1966) Mineralspektren II: Die Ultrarotabsorption Häufiger und Paragenetisch oder Wirtschaftlich Wichtiger Carbonate-, Borat-, Sulfat-, Chromat-, Phosphat-, Arsenat-, und Vanadat- und Silikatmineralien im Spektralbereich 400–4000 cm–1 (25–2.5 microns). Akademie Verlag, Berlin.Google Scholar
Moersch, J.E. & Christensen, P.R. (1995) Thermal emission from particulate surfaces: A comparison of scattering models with measured spectra. Journal of Geophysical Research, 100, 74657477.CrossRefGoogle Scholar
Morlok, A., Bowey, J., Köhler, M., & Grady, M.M. (2006) FTIR 2–16 micron spectroscopy of micron-sized olivines from primitive meteorites. Meteoritics and Planetary Science, 41, 773784.CrossRefGoogle Scholar
Mozgawa, W., Krol, M., & Barczyk, K. (2011) FT-IR studies of zeolites from different structural groups. Chemik, 65, 667674.Google Scholar
Mustard, J.F. & Hays, J.E. (1997) Effects of hyperfine particles on reflectance spectra from 0.3 to 25 µm. Icarus, 125, 145163.CrossRefGoogle Scholar
Onomichi, M., Kudo, K., & Arai, T. (1971) Reflection spectra of calcite in far-infrared region. Journal of the Physical Society of Japan, 31, 1837.CrossRefGoogle Scholar
Palomba, E., Rotundi, A., & Colangeli, L. (2006) Infrared micro-spectroscopy of the martian meteorite Zagami: Extraction of individual mineral phase spectra. Icarus, 182, 6879.CrossRefGoogle Scholar
Pieters, C.M. & Hiroi, T. (2004) RELAB (Reflectance Experiment Laboratory): A NASA multiuser spectroscopy facility. 35th Lunar Planet. Sci. Conf., Abstract #1720.
Pieters, C.M., Klima, R.L., Hiroi, T., et al. (2008) Martian dunite NWA 2737: Integrated spectroscopic analyses of brown olivine. Journal of Geophysical Research, 113, E06004, DOI:10.1029/2007JE002939.CrossRefGoogle Scholar
Pitman, K.M., Dijkstra, C., Hofmeister, A.M., & Speck, A.K. (2010) Infrared laboratory absorbance spectra of olivine: Using classical dispersion analysis to extract peak parameters. Mon. Royal Astronomical Society, 406, 460481.CrossRefGoogle Scholar
Pitman, K.M., Noe Dobrea, E.Z., Jamieson, C.S., Dalton III, J.B., Abbey, W.J., & Joseph, E.C.S. (2014) Reflectance spectroscopy and optical functions for hydrated Fe-sulfates. American Mineralogist, 99, 15931603.CrossRefGoogle Scholar
Ramsey, M.S. & Christensen, P.R. (1998) Mineral abundance determination: Quantitative deconvolution of thermal emission spectra. Journal of Geophysical Research, 103, 577596.CrossRefGoogle Scholar
Rogers, A.D. & Nekvasil, H. (2015) Feldspathic rocks on Mars: Compositional constraints from infrared spectroscopy and possible formation mechanisms. Geophysical Research Letters, 42, 26192626.CrossRefGoogle Scholar
Ross, S.D. (1974a) Sulphates and other oxy-anions of Group VI. In: The Infrared Spectra of Minerals (Farmer, V.C., ed.). The Mineralogical Society, London, 423444.CrossRefGoogle Scholar
Ross, S.D. (1974b) Phosphates and other oxyanions of Group V. In: The Infrared Spectra of Minerals (Farmer, V.C., ed.). The Mineralogical Society, London, 383422.CrossRefGoogle Scholar
Ruff, S.W. (2004) Spectral evidence for zeolite in the dust on Mars. Icarus, 168, 131143.CrossRefGoogle Scholar
Ruff, S.W. & Christensen, P.R. (2007) Basaltic andesite, altered basalt, and a TES-based search for smectite clay minerals on Mars. Geophysical Research Letters, 34, DOI:10.1029/2007GL029602.CrossRefGoogle Scholar
Ruff, S.W., Christensen, P.R., Barbera, P.W., & Anderson, D.L. (1997) Quantitative thermal emission spectroscopy of minerals: A technique for measurement and calibration. Journal of Geophysical Research, 102, 1489914913.CrossRefGoogle Scholar
Salisbury, F.B. & D’Aria, D.M. (1992) Emissivity of terrestrial materials in the 8–14 µm atmospheric window. Remote Sensing Environment, 42, 83106.CrossRefGoogle Scholar
Salisbury, J.W. & Eastes, J.W. (1985) The effect of particle size and porosity on spectral contrast in the mid-infrared. Icarus, 64, 586588.CrossRefGoogle Scholar
Salisbury, J.W. & Wald, A. (1992) The role of volume scattering in reducing spectral contrast of reststrahlen bands in spectra of powdered minerals. Icarus, 96, 121128.CrossRefGoogle Scholar
Salisbury, J.W. & Walter, L.S. (1989) Thermal infrared (2.5–13.5 µm) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces. Journal of Geophysical Research, 94, 91929202.CrossRefGoogle Scholar
Salisbury, J.W., Walter, L.S., & D’Aria, D. (1988) Mid-infrared (2.5 to 13.5 µm) spectra of igneous rocks. USGS Open File Report 88–686.
Salisbury, J.W., D’Aria, D.M., & Jarosewich, E. (1991a) Midinfrared (2.5–13.5 µm) reflectance spectra of powdered stony meteorites. Icarus, 92, 280297.CrossRefGoogle Scholar
Salisbury, J.W., Walter, L.S., Vergo, N., & D’Aria, D.M. (1991b) Infrared (2.1–25 µm) spectra of minerals. Johns Hopkins University Press, Baltimore, MD.Google Scholar
Salisbury, J.W., Wald, A., & D’Aria, D.M. (1994) Thermal-infrared remote sensing and Kirchhoff’s law 1. Laboratory measurements. Journal of Geophysical Research, 99, DOI:10.1029/93JB03600.CrossRefGoogle Scholar
Spitzer, W.G. & Kleinman, D.A. (1961) Infrared lattice bands of quartz. Physical Review, 121, 13241335.CrossRefGoogle Scholar
Stutman, J.M., Termine, J.D., & Posner, A.S. (1965) Vibrational spectra and the structure of the phosphate ion in some calcium phosphates. Transactions of the New York Academy of Sciences, 27, 669675, DOI:10.1111/j.2164-0947.CrossRefGoogle ScholarPubMed
Thomas, I.R., Greenhagen, B.T., Bowles, N.E., Donaldson Hanna, K.L., Temple, J., & Calcutt, S.B. (2012) A new experimental setup for making thermal emission measurements in a simulated lunar environment. Review of Scientific Instruments, 83, 124502.CrossRefGoogle Scholar
Vernazza, P., Delbo, M., King, P.L., et al. (2012) High surface porosity as the origin of emissivity features in asteroid spectra. Icarus, 221, 11621172.CrossRefGoogle Scholar
Vernazza, P., Castillo-Rogez, J., Beck, P., et al. (2017) Different origins or different evolutions? Decoding the spectral diversity among C-type asteroids. The Astronomical Journal, 153, 72.CrossRefGoogle Scholar
Wald, A.E. & Salisbury, J.W. (1995) Thermal infrared directional emissivity of powdered quartz. Journal of Geophysical Research, 100, 2466524675.CrossRefGoogle Scholar
Weinger, B.A., Reffner, J.A., & DeForest, P.R. (2009) A novel approach to the examination of soil evidence: Mineral identification using infrared microprobe analysis. Journal of Forensic Sciences, 54, 851856.CrossRefGoogle ScholarPubMed
Weir, C.E. & Lippincott, E.R. (1961) Infrared studies of aragonite, calcite, and vaterite type structures in the borates, carbonates, and nitrates. Journal of Research of the National Bureau of Standards A: Physics and Chemistry, 65A, 173183.CrossRefGoogle Scholar
Wenrich, M.L. & Christensen, P.R. (1996) Optical constants of minerals derived from emission spectroscopy: Application to quartz. Journal of Geophysical Research, 101, 1592115931.CrossRefGoogle Scholar
Wyatt, M.B., Hamilton, V.E., McSween, H.Y. Jr., Christensen, P.R., & Taylor, L.A. (2001) Analysis of terrestrial and martian volcanic compositions using thermal emission spectroscopy, 1. Determination of mineralogy, chemistry, and classification strategies. Journal of Geophysical Research, 106, 14,71114,732.CrossRefGoogle Scholar
Yesiltas, M., Sedlmair, J., & Peale, R.E. (2017) Synchrotron-based three-dimensional Fourier-transform infrared spectro-microtomography of Murchison meteorite grain. Applied Spectroscopy, 71(6), 11981208.CrossRefGoogle ScholarPubMed

References

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. Journal of Geophysical Research, 79, 48294836.CrossRefGoogle Scholar
Adams, J.B. (1975) Interpretation of visible and near-infrared diffuse reflectance spectra of pyroxenes and other rock-forming minerals. In: Infrared and Raman spectroscopy of lunar and terrestrial minerals (Karr, C., ed.). Academic Press, New York, 91116.CrossRefGoogle Scholar
Adams, J.B. & Filice, A.L. (1967) Spectral reflectance 0.4 to 2.0 microns of silicate rock powders. Journal of Geophysical Research, 72, 57055715.CrossRefGoogle Scholar
Adams, J.B. & Goullaud, L.H. (1978) Plagioclase feldspars: Visible and near infrared diffuse reflectance spectra as applied to remote sensing. Proceedings of the 9th Lunar and Planetary Science Conference, 29012909.
Allen, C.C., Gooding, J.L., Jercinovic, M., & Keil, K. (1981) Altered basaltic glass: A terrestrial analog to the soil of Mars. Icarus, 45, 347369.CrossRefGoogle Scholar
Amador, E.S., Bishop, J.L., McKeown, N.K., Parente, M., & Clark, J.T. (2009) Detection of Kaolinite at Mawrth Vallis, Mars: Analysis of laboratory mixtures and development of remote sensing parameters. 40th Lunar Planet. Sci. Conf., Abstract #2188.
Anderson, J.H. & Wickersheim, K.A. (1964) Near infrared characterization of water and hydroxyl groups on silica surfaces. Surface Science, 2, 252260.CrossRefGoogle Scholar
Baker, L.L., Strawn, D.G., McDaniel, P.A., et al. (2011) Poorly crystalline, iron-bearing aluminosilicates and their importance on Mars. 42nd Lunar Planet. Sci. Conf., Abstract #1939.
Bell, J.F., III, Morris, R.V. & Adams, J.B. (1993) Thermally altered palagonitic tephra: A spectral and process analog to the soil and dust of Mars. Journal of Geophysical Research, 98, 33733385.CrossRefGoogle Scholar
Bigham, J.M., Schwertmann, U., Traina, S.J., Winland, R.L., & Wolf, M. (1996) Schwertmannite and the chemical modeling of iron in acid sulfate waters. Geochimica Cosmochimica Acta, 60, 21112121.CrossRefGoogle Scholar
Bish, D. & Carey, J.W. (2001) Thermal behavior of natural zeolites. In: Natural zeolites: Occurrence, properties, and applications. Mineralogical Society of America Reviews in Mineralogy and Geochemistry (Bish, D.L. & Ming, D.W., eds.). Mineralogical Society of America, Washington, DC, 403–452.CrossRefGoogle Scholar
Bish, D.L., Carey, J.W., Vaniman, D.T., & Chipera, S.J. (2003) Stability of hydrous minerals on the martian surface. Icarus, 164, 96103.CrossRefGoogle Scholar
Bishop, J.L. (2005) Hydrated minerals on Mars. In: Water on Mars and life. Advances in Astrobiology and Biogeophysics. (Tokano, T., ed.). Springer, Berlin, 65–96.Google Scholar
Bishop, J.L. & Murad, E. (1996) Schwertmannite on Mars? Spectroscopic analyses of schwertmannite, its relationship to other ferric minerals, and its possible presence in the surface material on Mars. In: Mineral spectroscopy: A tribute to Roger G. Burns (Dyar, M.D., McCammon, C., & Schaefer, M.W., eds.). The Geochemical Society, Houston, TX, 337358.Google Scholar
Bishop, J.L. & Murad, E. (2002) Spectroscopic and geochemical analyses of ferrihydrite from hydrothermal springs in Iceland and applications to Mars. In: Volcano–ice interactions on Earth and Mars (Smellie, J.L. & Chapman, M.G., eds.). Special Publication No.202. Geological Society, London, 357370.Google Scholar
Bishop, J.L. & Murad, E. (2005) The visible and infrared spectral properties of jarosite and alunite. American Mineralogist, 90, 11001107.CrossRefGoogle Scholar
Bishop, J.L. & Pieters, C.M. (1995) Low-temperature and low atmospheric pressure infrared reflectance spectroscopy of Mars soil analog materials. Journal of Geophysical Research, 100, 53695379.CrossRefGoogle Scholar
Bishop, J.L. & Rampe, E.B. (2016) Evidence for a changing martian climate from the mineralogy at Mawrth Vallis. Earth and Planetary Science Letters, 448, 4248.CrossRefGoogle Scholar
Bishop, J.L., Pieters, C.M., & Burns, R.G. (1993) Reflectance and Mössbauer spectroscopy of ferrihydrite-montmorillonite assemblages as Mars soil analog materials. Geochimica Cosmochimica Acta, 57, 45834595.CrossRefGoogle ScholarPubMed
Bishop, J.L., Pieters, C.M., & Edwards, J.O. (1994) Infrared spectroscopic analyses on the nature of water in montmorillonite. Clays and Clay Minerals, 42, 702716.CrossRefGoogle Scholar
Bishop, J.L., Fröschl, H., & Mancinelli, R.L. (1998a) Alteration processes in volcanic soils and identification of exobiologically important weathering products on Mars using remote sensing. Journal of Geophysical Research, 103, 31,45731,476.CrossRefGoogle ScholarPubMed
Bishop, J.L., Pieters, C.M., Hiroi, T., & Mustard, J.F. (1998b) Spectroscopic analysis of martian meteorite Allan Hills 84001 powder and applications for spectral identification of minerals and other soil components on Mars. Meteoritics and Planetary Science, 33, 699708.CrossRefGoogle Scholar
Bishop, J.L., Mustard, J.F., Pieters, C.M., & Hiroi, T. (1998c) Recognition of minor constituents in reflectance spectra of Allan Hills 84001 chips and the importance for remote sensing on Mars. Meteoritics and Planetary Science, 33, 693698.CrossRefGoogle Scholar
Bishop, J.L., Murad, E., Madejová, J., Komadel, P., Wagner, U., & Scheinost, A. (1999) Visible, Mössbauer and infrared spectroscopy of dioctahedral smectites: Structural analyses of the Fe-bearing smectites Sampor, SWy-1 and SWa-1. 11th International Clay Conference, June, 1997 (Kodama, H., Mermut, A.R., & Torrance, J.K., eds.). Ottawa, 413419.
Bishop, J.L., Lougear, A., Newton, J., et al. (2001) Mineralogical and geochemical analyses of Antarctic sediments: A reflectance and Mössbauer spectroscopy study with applications for remote sensing on Mars. Geochimica Cosmochimica Acta, 65, 28752897.CrossRefGoogle Scholar
Bishop, J.L., Schiffman, P., & Southard, R.J. (2002a) Geochemical and mineralogical analyses of palagonitic tuffs and altered rinds of pillow lavas on Iceland and applications to Mars. In: Volcano–ice interactions on Earth and Mars (Smellie, J.L. & Chapman, M.G., eds.). Special Publication No. 202. Geological Society, London, 371392.Google Scholar
Bishop, J.L., Murad, E., & Dyar, M.D. (2002b) The influence of octahedral and tetrahedral cation substitution on the structure of smectites and serpentines as observed through infrared spectroscopy. Clay Minerals, 37, 617628.CrossRefGoogle Scholar
Bishop, J.L., Madeová, J., Komadel, P., & Fröschl, H. (2002c) The influence of structural Fe, Al and Mg on the infrared OH bands in spectra of dioctahedral smectites. Clay Minerals, 37, 607616.CrossRefGoogle Scholar
Bishop, J.L., Minitti, M.E., Lane, M.D., & Weitz, C.M. (2003) The influence of glassy coatings on volcanic rocks from Mauna Iki, Hawaii and applications to rocks on Mars. 34th Lunar Planet. Sci. Conf., Abstract #1516.
Bishop, J.L., Murad, E., Lane, M.D., & Mancinelli, R.L. (2004) Multiple techniques for mineral identification on Mars: A study of hydrothermal rocks as potential analogues for astrobiology sites on Mars. Icarus, 169, 331–323.Google Scholar
Bishop, J.L., Dyar, M.D., Lane, M.D., & Banfield, J.F. (2005) Spectral identification of hydrated sulfates on Mars and comparison with acidic environments on Earth. International Journal of Astrobiology, 3, 275285.CrossRefGoogle Scholar
Bishop, J.L., Schiffman, P., Murad, E., Dyar, M.D., Drief, A., & Lane, M.D. (2007) Characterization of alteration products in tephra from Haleakala, Maui: A visible-infrared spectroscopy, Mössbauer spectroscopy, XRD, EPMA and TEM study. Clays and Clay Minerals, 55, 117.CrossRefGoogle Scholar
Bishop, J.L., Dyar, M.D., Sklute, E.C., & Drief, A. (2008a) Physical alteration of antigorite: A Mössbauer spectroscopy, reflectance spectroscopy and TEM study with applications to Mars. Clay Minerals, 43, 5567.CrossRefGoogle Scholar
Bishop, J.L., Lane, M.D., Dyar, M.D., & Brown, A.J. (2008b) Reflectance and emission spectroscopy study of four groups of phyllosilicates: Smectites, kaolinite-serpentines, chlorites and micas. Clay Minerals, 43, 3554.CrossRefGoogle Scholar
Bishop, J.L., Parente, M., Weitz, C.M., et al. (2009) Mineralogy of Juventae Chasma: Sulfates in the light-toned mounds, mafic minerals in the bedrock, and hydrated silica and hydroxylated ferric sulfate on the plateau. Journal of Geophysical Research, 114, E00D09, DOI:10.1029/2009JE003352.CrossRef
Bishop, J.L., Parente, M., & Hamilton, V.E. (2011a) Spectral signatures of martian meteorites and what they can tell us about rocks on Mars. Meteoritical Society 74th Annual Meeting, Abstract #5393.
Bishop, J.L., Gates, W.P., Makarewicz, H.D., McKeown, N.K., & Hiroi, T. (2011b) Reflectance spectroscopy of beidellites and their importance for Mars. Clays and Clay Minerals, 59, 376397.CrossRefGoogle Scholar
Bishop, J.L., Schelble, R.T., McKay, C.P., Brown, A.J., & Perry, K.A. (2011c) Carbonate rocks in the Mojave Desert as an analog for martian carbonates. International Journal of Astrobiology, 10, 349358, DOI:10.1017/S1473550411000206.CrossRefGoogle Scholar
Bishop, J.L., Perry, K.A., Dyar, M.D., et al. (2013a) Coordinated spectral and XRD analyses of magnesite-nontronite-forsterite mixtures and implications for carbonates on Mars. Journal of Geophysical Research, 118, 635650.Google Scholar
Bishop, J.L., Rampe, E.B., Bish, D.L., et al. (2013b) Spectral and hydration properties of allophane and imogolite. Clays and Clay Minerals, 61, 5774.CrossRefGoogle Scholar
Bishop, J.L., Quinn, R.C., & Dyar, M.D. (2014a) Spectral and thermal properties of perchlorate salts and implications for Mars. American Mineralogist, 99, 15801592.CrossRefGoogle Scholar
Bishop, J.L., Lane, M.D., Dyar, M.D., King, S.J., Brown, A.J., & Swayze, G. (2014b) Spectral properties of Ca-sulfates: Gypsum, bassanite and anhydrite. American Mineralogist, 99, 21052115.CrossRefGoogle Scholar
Bishop, J.L., Murad, E., & Dyar, M.D. (2015) Akaganéite and schwertmannite: Spectral properties, structural models and geochemical implications of their possible presence on Mars. American Mineralogist, 100, 738746.CrossRefGoogle Scholar
Bishop, J.L., Davila, A., Hanley, J., & Roush, T.L. (2016a) Dehydration-rehydration experiments with Cl salts mixed into Mars analog materials and the effects on their VNIR spectral properties. 47th Lunar Planet. Sci. Conf., Abstract #1645.
Bishop, J.L., Schiffman, P., Gruendler, L., et al. (2016b) Formation of opal, clays and sulfates from volcanic ash at Kilauea Caldera as an analog for surface alteration on Mars. Clay Minerals Society 53rd Annual Meeting.
Bishop, J.L., King, S.J., Lane, M.D., et al. (2017) Spectral properties of anhydrous carbonates and nitrates. 48th Lunar Planet. Sci. Conf., Abstract #2362.
Bishop, J.L., King, S.J., Lane, M.D., et al. (2019) Spectral properties of anhydrous carbonates and nitrates. Journal of Geophysical Research, submitted.
Brindley, G.W. & Brown, G. (1980) Crystal structures of clay minerals and their X-ray identification. Mineralogical Society, London.CrossRefGoogle Scholar
Burns, R.G. (1970) Crystal field spectra and evidence of cation ordering in olivine minerals. American Mineralogist, 55, 16081632.Google Scholar
Burns, R.G. (1993) Mineralogical applications of crystal field theory. Cambridge University Press, Cambridge.CrossRefGoogle Scholar
Burns, R.G. & Huggins, F.E. (1972) Cation determinative curves for Mg-Fe-Mn olivines from vibrational spectra. American Mineralogist, 57, 967985.Google Scholar
Calvin, W.M. & King, T.V.V. (1997) Spectral characteristics of Fe-bearing phyllosilicates: Comparison to Orgueil (C11), Murchison and Murray (CM2). Meteoritics and Planetary Science, 32, 693701.CrossRefGoogle Scholar
Calvin, W.M., King, T.V.V., & Clark, R.N. (1994) Hydrous carbonates on Mars? Evidence from Mariner 6/7 infrared spectrometer and groundbased telescopic spectra. Journal of Geophysical Research, 99, 1465914675.CrossRefGoogle Scholar
Cannon, K.M., Mustard, J.F., Parman, S.W., Sklute, E.C., Dyar, M.D., & Cooper, R.F. (2017) Spectral properties of martian and other planetary glasses and their detection in remotely sensed data. Journal of Geophysical Research, 122, 249268.Google Scholar
Cariati, F., Erre, L., Gessa, C., Micera, G., & Piu, P. (1981) Water molecules and hydroxyl groups in montmorillonites as studied by near infrared spectroscopy. Clays and Clay Minerals, 29, 157159.CrossRefGoogle Scholar
Chapman, C.R. & Salisbury, J.W. (1973) Comparisons of meteorite and asteroid spectral reflectivities. Icarus, 19, 507522.CrossRefGoogle Scholar
Cheek, L.C., Pieters, C.M., Dyar, M.D., & Milam, K.A. (2009) Revisiting plagioclase optical properties for lunar exploration. 40th Lunar Planet. Sci. Conf., Abstract #1928.
Clark, J.T., Bishop, J.L., Parente, M., Brown, A.J., & McKeown, N.K. (2008) Constraining sulfate abundances on Mars using CRISM spectra and laboratory mixtures. 39th Lunar Planet. Sci. Conf., Abstract #1540.
Clark, R.N. (1983) Spectral properties of mixtures of montmorillonite and dark carbon grains: Implications for remote sensing minerals containing chemically and physically adsorbed water. Journal of Geophysical Research, 88, 1063510644.CrossRefGoogle Scholar
Clark, R.N. (1999) Spectroscopy of rocks and minerals, and principles of spectroscopy. In: Manual of remote sensing, 3: Remote sensing for the Earth sciences (Rencz, A.N., ed.). John Wiley & Sons, New York, 358.Google Scholar
Clark, R.N. & Roush, T.L. (1984) Reflectance spectroscopy: Quantitative analysis techniques for remote sensing applications. Journal of Geophysical Research, 89, 63296340.CrossRefGoogle Scholar
Clark, R.N., King, T.V.V., Klejwa, M., & Swayze, G.A. (1990) High spectral resolution reflectance spectroscopy of minerals. Journal of Geophysical Research, 95, 1265312680.CrossRefGoogle Scholar
Clark, R.N., Swayze, G.A., Livo, K.E., et al. (2003) Imaging spectroscopy: Earth and planetary remote sensing with the USGS Tetracorder and expert systems. Journal of Geophysical Research, 108, 5131, DOI:10.1029/2002JE001847.CrossRefGoogle Scholar
Cloutis, E.A. & Gaffey, M.J. (1991) Pyroxene spectroscopy revisited: Spectral-compositional correlations and relationships to geothermometry. Journal of Geophysical Research, 96, 2280922826.CrossRefGoogle Scholar
Cloutis, E.A., Gaffey, M.J., Jackowski, T., & Reed, K. (1986) Calibration of phase abundance, composition, and particle size distribution for olivine-orthopyroxene mixtures from reflectance spectra. Journal of Geophysical Research, 91, 1164111653.CrossRefGoogle Scholar
Cloutis, E.A., Asher, P.M., & Mertzman, S.A. (2002) Spectral reflectance properties of zeolites and remote sensing implications. Journal of Geophysical Research, 107, 5067, DOI:10.1029/2000JE001467.CrossRefGoogle Scholar
Cloutis, E.A., Sunshine, J.M., & Morris, R.V. (2004) Spectral reflectance-compositional properties of spinels and chromites: Implications for planetary remote sensing and geothermometry. Meteoritics and Planetary Science, 39, 545565.CrossRefGoogle Scholar
Cloutis, E.A., Hawthorne, F.C., Mertzman, S.A., et al. (2006) Detection and discrimination of sulfate minerals using reflectance spectroscopy. Icarus, 184, 121157.CrossRefGoogle Scholar
Cloutis, E.A., Craig, M.A., Kruzelecky, R.V., et al. (2008) Spectral reflectance properties of minerals exposed to simulated Mars surface conditions. Icarus, 195, 140168.CrossRefGoogle Scholar
Cloutis, E.A., Hardersen, P.S., Bish, D.L., Bailey, D.T., Gaffey, M.J., & Craig, M.A. (2010a) Reflectance spectra of iron meteorites: Implications for spectral identification of their parent bodies. Meteoritics and Planetary Science, 45, 304332.CrossRefGoogle Scholar
Cloutis, E.A., Hudon, P., Romanek, C.S., et al. (2010b) Spectral reflectance properties of ureilites. Meteoritics and Planetary Science, 45, 16681694.CrossRefGoogle Scholar
Cloutis, E.A., Hiroi, T., Gaffey, M.J., Alexander, C.M.O.D., & Mann, P. (2011a) Spectral reflectance properties of carbonaceous chondrites: 1. CI chondrites. Icarus, 212, 180209.CrossRefGoogle Scholar
Cloutis, E.A., Hudon, P., Hiroi, T., Gaffey, M.J., & Mann, P. (2011b) Spectral reflectance properties of carbonaceous chondrites: 2. CM chondrites. Icarus, 216, 309346.CrossRefGoogle Scholar
Cloutis, E.A., Hudon, P., Hiroi, T., & Gaffey, M.J. (2012a) Spectral reflectance properties of carbonaceous chondrites: 3. CR chondrites. Icarus, 217, 389407.CrossRefGoogle Scholar
Cloutis, E.A., Hudon, P., Hiroi, T., & Gaffey, M.J. (2012b) Spectral reflectance properties of carbonaceous chondrites: 7. CK chondrites. Icarus, 221, 911924.CrossRefGoogle Scholar
Cloutis, E.A., Hudon, P., Hiroi, T., Gaffey, M.J., & Mann, P. (2012c) Spectral reflectance properties of carbonaceous chondrites: 8. “Other” carbonaceous chondrites: CH, ungrouped, polymict, xenolithic inclusions, and R chondrites. Icarus, 221, 9841001.CrossRefGoogle Scholar
Cloutis, E., Berg, B., Mann, P., & Applin, D. (2016) Reflectance spectroscopy of low atomic weight and Na-rich minerals: Borates, hydroxides, nitrates, nitrites, and peroxides. Icarus, 264, 2036.CrossRefGoogle Scholar
Cornell, R.M. & Schwertmann, U. (2003) The iron oxides: Structure, properties, reactions, occurrences and uses, 2nd edn. Wiley-VCH, Weinheim.CrossRefGoogle Scholar
Cotton, F.A. (1990) Chemical applications of group theory, 3rd edn. Wiley-Interscience, New York.Google Scholar
Crowley, J.K. (1991) Visible and near-infrared (0.4–2.5 μm) reflectance spectra of Playa evaporite minerals. Journal of Geophysical Research, 96, 1623116240.CrossRefGoogle Scholar
Crowley, J.K., Williams, D.E., Hammarstrom, J.M., Piatak, N., Chou, I.-M. & Mars, J.C. (2003) Spectral reflectance properties (0.4–2.5 µm) of secondary Fe-oxide, Fe-hydroxide, and Fe-sulphate-hydrate minerals associated with sulphide-bearing mine wastes. Geochemistry: Exploration, Environment, Analysis, 3, 219228.Google Scholar
Cuadros, J., Michalski, J.R., Dekov, V., Bishop, J., Fiore, S., & Dyar, M.D. (2013) Crystal-chemistry of interstratified Mg/Fe-clay minerals from seafloor hydrothermal sites. Chemical Geology, 360361, 142158.CrossRefGoogle Scholar
Dalton, J.B. (2003) Spectral behavior of hydrated sulfate salts: Implications for Europa Mission spectrometer design. Astrobiology, 3, 771784.CrossRefGoogle ScholarPubMed
Davis, A.C., Bishop, J.L., Veto, M., et al. (2014) Comparing VNIR and TIR spectra of clay-bearing rocks. 45th Lunar Planet. Sci. Conf., Abstract #2699.
De Angelis, S., Manzari, P., De Sanctis, M.C., Ammannito, E., & Di Iorio, T. (2016) VIS-IR study of brucite–clay–carbonate mixtures: Implications for Ceres surface composition. Icarus, 280, 315327.CrossRefGoogle Scholar
Decarreau, A., Petit, S., Martin, F., Vieillard, P., & Joussein, E. (2008) Hydrothermal synthesis, between 75 and 150C, of high-charge ferric nontronites. Clays and Clay Mineral, 56, 322337.CrossRefGoogle Scholar
Deer, W.A., Howie, R.A., & Zussman, J. (1992) An introduction to the rock-forming minerals. Longman, London.Google Scholar
Dyar, M.D., Sklute, E.C., Menzies, O.N., et al. (2009) Spectroscopic characteristics of synthetic olivine: An integrated multi-wavelength and multi-technique approach. American Mineralogist, 94, 883898.CrossRefGoogle Scholar
Ehlmann, B.L., Mustard, J.F., & Poulet, F. (2009) Modeling modal mineralogy of laboratory mixtures of nontronite and mafic minerals from visible near-infrared spectra data. 40th Lunar Planet. Sci. Conf., Abstract #1771.
Ehlmann, B.L., Bish, D.L., Ruff, S.W., & Mustard, J.F. (2012) Mineralogy and chemistry of altered Icelandic basalts: Application to clay mineral detection and understanding aqueous environments on Mars. Journal of Geophysical Research, 117, E00J16, DOI:10.1029/2012JE004156.CrossRefGoogle Scholar
Farrand, W.H. & Singer, R.B. (1992) Alteration of hydrovolcanic basaltic ash: Observations with visible and near-infrared spectrometry. Journal of Geophysical Research, 97, 1739317408.CrossRefGoogle Scholar
Fernandez-Martinez, A., Timon, V., Roman-Ross, G., Cuello, G.J., Daniels, J.E., & Ayora, C. (2010) The structure of schwertmannite, a nanocrystalline iron oxyhydroxysulfate. American Mineralogist, 95, 13121322.CrossRefGoogle Scholar
Fischer, E. & Pieters, C.M. (1993) The continuum slope of Mars: Bi-directional reflectance investigations and applications to Olympus Mons. Icarus, 102, 185202.CrossRefGoogle Scholar
Fraeman, A.A., Ehlmann, B.L., Northwood-Smith, G.W.D., Liu, Y., Wadhwa, M., & Greenberger, R.N. (2016) Using VSWIR microimaging spectroscopy to explore the mineralogical diversity of HED meteorites. 8th Workshop on Hyperspectral Image and Signal Processing: Evolution in Remote Sensing (WHISPERS), 1–5.
Gaffey, M.J. (1976) Spectral reflectance characteristics of the meteorite classes. Journal of Geophysical Research, 81, 905920.CrossRefGoogle Scholar
Gaffey, S.J. (1987) Spectral reflectance of carbonate minerals in the visible and near infared (0.35–2.55 µm): Anhydrous carbonate minerals. Journal of Geophysical Research, 92, 14291440.CrossRefGoogle Scholar
Gaffey, S.J., McFadden, L.A., Nash, D. & Pieters, C.M. (1993) Ultraviolet, visible, and near-infrared reflectance spectroscopy: Laboratory spectra of geologic materials. In: Remote geochemical analysis: Elemental and mineralogical composition (Pieters, C.M & Englert, P.A.J., eds.). Cambridge University Press, Cambridge, 4377.Google Scholar
Gates, W.P. (2005) Infrared spectroscopy and the chemistry of dioctahedral smectites. In: The application of vibrational spectroscopy to clay minerals and layered double hydroxides (Kloprogge, J.T., ed.). Clay Minerals Society, Aurora, CO, 125168.Google Scholar
Goryniuk, M.C., Rivard, B.A., & Jones, B. (2004) The reflectance spectra of opal-A (0.5–25 μm) from the Taupo Volcanic Zone: Spectra that may identify hydrothermal systems on planetary surfaces. Geophysical Research Letters, 31, DOI:10.1029/2004GL021481.CrossRefGoogle Scholar
Hanley, J., Dalton, J.B., Chevrier, V.F., Jamieson, C.S., & Barrows, R.S. (2014) Reflectance spectra of hydrated chlorine salts: The effect of temperature with implications for Europa. Journal of Geophysical Research, 119, 23702377.Google Scholar
Hanley, J., Chevrier, V.F., Barrows, R.S., Swaffer, C., & Altheide, T.S. (2015) Near- and mid-infrared reflectance spectra of hydrated oxychlorine salts with implications for Mars. Journal of Geophysical Research, 120, 14151426.Google Scholar
Hapke, B. (1993) Theory of reflectance and emittance spectroscopy. Cambridge University Press, Cambridge.CrossRefGoogle Scholar
Harner, P.L. & Gilmore, M.S. (2015) Visible–near infrared spectra of hydrous carbonates, with implications for the detection of carbonates in hyperspectral data of Mars. Icarus, 250, 204214.CrossRefGoogle Scholar
Herzberg, G. (1945) Molecular spectra and molecular structure. II. Infrared and Raman spectra of polyatomic molecules. D. Van Nostrand, New York.Google Scholar
Hiroi, T. & Pieters, C.M. (1994) Estimation of grain sizes and mixing ratios of fine powder mixtures of common geologic minerals. Journal of Geophysical Research, 99, 10,86710,879.CrossRefGoogle Scholar
Hiroi, T., Miyamoto, M., Mikouchi, T., & Ueda, Y. (2005) Visible and near-infrared reflectance spectroscopy of the Yamato 980459 meteorite in comparison with some shergottites. Antarctic Metorite Research, 18, 8395.Google Scholar
Hiroi, T., Jenniskens, P.M., Bishop, J.L., Shatir, T.S.M., Kudoda, A.M., & Shaddad, M.H. (2010) Bidirectional visible-NIR and biconical FT-IR reflectance spectra of Almahata Sitta meteorite samples. Meteoritics and Planetary Science, 45, 18361845.CrossRefGoogle Scholar
Honma, A., Bishop, J.L., McKeown, N.K., Brown, A.J., & Parente, M. (2008) Constraining phyllosilicate abundances on Mars using CRISM spectra and laboratory mixtures. 39th Lunar Planet. Sci. Conf., Abstract #1457.
Huheey, J.E., Keiter, E.A., & Keiter, R.I. (1993) lnorganic chemistry: Principles of structure and reactivity, 4th edn. HarperCollins, New York.Google Scholar
Hunt, G.R. & Ashley, R.P. (1979) Spectra of altered rocks in the visible and near infrared. Economic Geology, 74, 16131629.CrossRefGoogle Scholar
Hunt, G.R. & Salisbury, J.W. (1970) Visible and near-infrared spectra of minerals and rocks: 1. Silicate minerals. Modern Geology, 1, 283300.Google Scholar
Hunt, G.R. & Salisbury, J.W. (1971) Visible and near-infrared spectra of minerals and rocks: II. Carbonates. Modern Geology, 2, 2330.Google Scholar
Hunt, G.R., Salisbury, J.W., & Lenhoff, C.J. (1971a) Visible and near-infrared spectra of minerals and rocks: III. Oxides and hydroxides. Modern Geology, 2, 195205.Google Scholar
Hunt, G.R., Salisbury, J.W., & Lenhoff, C.J. (1971b) Visible and near-infrared spectra of minerals and rocks: IV. Sulphides and sulphates. Modern Geology, 3, 114.Google Scholar
Isaacson, P.J., Liu, Y., Patchen, A., Pieters, C.M., & Taylor, L.A. (2009) Integrated analyses of Lunar meteorites: Expanded data for lunar ground truth. 40th Lunar Planet. Sci. Conf., Abstract #2119.
Isaacson, P.J., Liu, Y., Patchen, A.D., Pieters, C.M., & Taylor, L.A. (2010) Spectroscopy of Lunar meteorites as constraints for ground truth: Expanded sample collection diversity. 41st Lunar Planet. Sci. Conf., Abstract #1927.
Isaacson, P.J., Basu Sarbadhikari, A., Pieters, C.M., et al. (2011) The lunar rock and mineral characterization consortium: Deconstruction and integrated mineralogical, petrologic, and spectroscopic analyses of mare basalts. Meteoritics and Planetary Science, 46, 228251.CrossRefGoogle Scholar
Isaacson, P.J., Klima, R.L., Sunshine, J.M., et al. (2014) Visible to near-infrared optical properties of pure synthetic olivine across the olivine solid solution. American Mineralogist, 99, 467478.CrossRefGoogle Scholar
Jenniskens, P., Shaddad, M.H., Numan, D., et al. (2009) The impact and recovery of asteroid 2008 TC3. Nature, 458, 485488.CrossRefGoogle Scholar
Jeute, T.J., Baker, L.L., Abidin, Z., Bishop, J.L., & Rampe, E.B. (2017) Characterizing nanophase materials on Mars: Spectroscopic studies of allophane and imogolite. 48th Lunar Planet. Sci. Conf., Abstract #2738.
Johnson, J.R. & Hörz, F. (2003) Visible/near-infrared spectra of experimentally shocked plagioclase feldspars. Journal of Geophysical Research, 108, 5120, DOI:10.1029/2003JE002127, E11.CrossRefGoogle Scholar
King, S.J., Bishop, J.L., Fenton, L.K., Lafuente, B., Garcia, G.C., & Horgan, B.H. (2013) VNIR reflectance spectra of gypsum mixtures for comparison with White Sands National Monument, New Mexico (WSNM) dune samples as an analog study of the Olympia Undae region of Mars. AGU Fall Meeting, Abstract #P23C-1800.
King, T.V.V. & Clark, R.N. (1989) Spectral characteristics of chlorites and Mg-serpentines using high-resolution reflectance spectroscopy. Journal of Geophysical Research, 94, 13,99714,008.CrossRefGoogle Scholar
Klima, R.L., Pieters, C.M., & Dyar, M.D. (2007) Spectroscopy of synthetic Mg-Fe pyroxenes I: Spin-allowed and spin-forbidden crystal field bands in the visible and near-infrared. Meteoritics and Planetary Science, 42, 235253.CrossRefGoogle Scholar
Klima, R.L., Pieters, C.M., & Dyar, M.D. (2008) Characterization of the 1.2 micrometer M1 pyroxene band: Extracting cooling history from near-IR spectra of pyroxenes and pyroxene-dominated rocks. Meteoritics and Planetary Science, 43, 15911604.CrossRefGoogle Scholar
Klima, R.L., Dyar, M.D., & Pieters, C.M. (2011) Near-infrared spectra of clinopyroxenes: effects of calcium content and crystal structure. Meteoritics and Planetary Science, 46, 379395.CrossRefGoogle Scholar
Lane, M.D. & Christensen, P.R. (1997) Thermal infrared emission spectroscopy of anhydrous carbonates. Journal of Geophysical Research, 102, 2558125592.CrossRefGoogle Scholar
Lane, M.D., Dyar, M.D., & Bishop, J.L. (2007) Spectra of phosphate minerals as obtained by visible-near infrared reflectance, thermal infrared emission, and Mössbauer laboratory analyses. 38th Lunar Planet. Sci. Conf., Abstract #2210.
Lane, M.D., Bishop, J.L., Dyar, M.D., et al. (2015) Mid-infrared emission spectroscopy and visible/near-infrared reflectance spectroscopy of Fe-sulfate minerals. American Mineralogist, 100, 6682.CrossRefGoogle Scholar
Lapotre, M.G.A., Ehlmann, B.L., & Minson, S.E. (2017) A probabilistic approach to remote compositional analysis of planetary surfaces. Journal of Geophysical Research, 122, 9831009.Google Scholar
Lauretta, D.S. & McSween, H.Y. Jr. (2006) Meteorites and the early solar system II. The University of Arizona Press, Tucson, AZ.Google Scholar
Lin, T.J., Ver Eecke, H.C., Breves, E.A., et al. (2016) Linkages between mineralogy, fluid chemistry, and microbial communities within hydrothermal chimneys from the Endeavour Segment, Juan de Fuca Ridge. Geochemistry, Geophysics, Geosystems, 17, 300323.CrossRefGoogle Scholar
McFadden, L.A. & Cline, T.P. (2005) Spectral reflectance of martian meteorites: Spectral signatures as a template for locating source region on Mars. Meteoritics and Planetary Science, 40, 151172.CrossRefGoogle Scholar
McFadden, L.A., Gaffey, M.J., & Takeda, H. (1980) Reflectance spectra of some newly found, unusual meteorites and their bearing on the surface mineralogy of asteroids. Proceedings of the 13th Lunar and Planetary Symposium, Tokyo, 273–280.
McKeown, N.K., Bishop, J.L., Cuadros, J., et al. (2011) Interpretation of reflectance spectra of clay mineral-silica mixtures: Implications for martian clay mineralogy at Mawrth Vallis. Clays and Clay Mineral, 59, 400415.CrossRefGoogle Scholar
Milliken, R.E. & Mustard, J.F. (2005) Quantifying absolute water content of minerals using near-infrared reflectance spectroscopy. Journal of Geophysical Research, 110, E12001, DOI:10.1029/2005JE002534.CrossRefGoogle Scholar
Milliken, R.E., Swayze, G.A., Arvidson, R.E., et al. (2008) Opaline silica in young deposits on Mars. Geology, 36, 847850.CrossRefGoogle Scholar
Minitti, M.E. & Rutherford, M.J. (2000) Genesis of the Mars Pathfinder “sulfur-free” rock from SNC parental liquids. Geochimica Cosmochimica Acta, 64, 25352547.CrossRefGoogle Scholar
Minitti, M.E., Mustard, J.F., & Rutherford, M.J. (2002) The effects of glass content and oxidation on the spectra of SNC-like basalts: Application to Mars remote sensing. Journal of Geophysical Research, 107(E5), DOI:10.1029/2001JE001518.CrossRef
Minitti, M.E., Weitz, C.M., Lane, M.D., & Bishop, J.L. (2007) Morphology, chemistry, and spectral properties of Hawaiian rock coatings and implications for Mars. Journal of Geophysical Research, 112, E05015, DOI: 10.1029/2006JE002839.CrossRefGoogle Scholar
Moroz, L., Schade, U., & Wäsch, R. (2000) Reflectance spectra of olivine-orthopyroxene-bearing assemblages at decreased temperatures: Implications for remote sensing of asteroids. Icarus, 147, 7993.CrossRefGoogle Scholar
Morris, R.V., Lauer, H.V. Jr., Lawson, C.A., Gibson, E.K. Jr., Nace, G.A., & Stewart, C. (1985) Spectral and other physicochemical properties of submicron powders of hematite (a-Fe2O3), maghemite (g-Fe2O3), magnetite (Fe3O4), goethite (a-FeOOH), and lepidocrocite (g-FeOOH). Journal of Geophysical Research, 90, 31263144.CrossRefGoogle Scholar
Morris, R.V., Agresti, D.G., Lauer, H.V. Jr., Newcomb, J.A., Shelfer, T.D., & Murali, A.V. (1989) Evidence for pigmentary hematite on Mars based on optical, magnetic and Mössbauer studies of superparamagnetic (nanocrystalline) hematite. Journal of Geophysical Research, 94, 27602778.CrossRefGoogle Scholar
Morris, R.V., Gooding, J.L., Lauer, H.V. Jr., & Singer, R.B. (1990) Origins of Marslike spectral and magnetic properties of a Hawaiian palagonitic soil. Journal of Geophysical Research, 95, 14,42714,434.CrossRefGoogle Scholar
Morris, R.V., Schulze, D.G., Lauer, H.V. Jr., Agresti, D.G., & Shelfer, T.D. (1992) Reflectivity (visible and near IR), Mössbauer, static magnetic, and X ray diffraction properties of aluminum-substituted hematites. Journal of Geophysical Research, 97, 1025710266.CrossRefGoogle Scholar
Morris, R.V., Golden, D.C., Bell, J.F. III, & Lauer, H.V. Jr. (1995) Hematite, pyroxene, and phyllosilicates on Mars: Implications from oxidized impact melt rocks from Manicouagan crater, Quebec, Canada. Journal of Geophysical Research, 100, 53195328.CrossRefGoogle Scholar
Morris, R.V., Golden, D.C., & Bell, J.F. III (1997) Low-temperature reflectivity spectra of red hematite and the color of Mars. Journal of Geophysical Research, 102, 91259133.CrossRefGoogle Scholar
Morris, R.V., Golden, D.C., Shelfer, T.D., & Lauer, H.V. Jr. (1998) Lepidocrocite to maghemite to hematite: A pathway to magnetic and hematitic martian soil. Meteoritics and Planetary Science, 33, 743751.CrossRefGoogle Scholar
Morris, R.V., Graff, T.G., Mertzman, S.A., Lane, M.D., & Christensen, P.R. (2003) Palagonitic (not Andesitic) Mars: Evidence from thermal emission and VNIR spectra of Palagonitic alteration rinds on basaltic rock. 6th Int. Conf. on Mars, Abstract #3211.
Mustard, J.F. (1992) Chemical analysis of actinolite from reflectance spectra. American Mineralogist, 77, 345358.Google Scholar
Mustard, J.F. & Hays, J.E. (1997) Effects of hyperfine particles on reflectance spectra from 0.3 to 25 µm. Icarus, 125, 145163.CrossRefGoogle Scholar
Mustard, J.F. & Pieters, C.M. (1987) Abundance and distribution of ultramafic microbreccia in moses rock dike: Quantitative application of mapping spectroscopy. Journal of Geophysical Research, 92, 1037610390.CrossRefGoogle Scholar
Mustard, J.F. & Pieters, C.M. (1989) Photometric phase functions of common geologic minerals and applications to quantitative analysis of mineral mixture reflectance spectra. Journal of Geophysical Research, 94, 1361913634.CrossRefGoogle Scholar
Mustard, J.F., Sunshine, J.M., Pieters, C.M., Hoppin, A., & Pratt, S.F. (1993) From minerals to rocks: Toward modeling lithologies with remote sensing. 24th Lunar Planet. Sci. Conf., Abstract, 1041–1042.
Mustard, J.F., Murchie, S.L., Erard, S., & Sunshine, J.M. (1997) In situ compositions of martian volcanics: Implications for the mantle. Journal of Geophysical Research, 102, 25,60525,615.CrossRefGoogle Scholar
Nash, D.B. & Conel, J.E. (1974) Spectral reflectance systematics for mixtures of powdered hypersthene, labradorite, and ilmenite. Journal of Geophysical Research, 79, 16151621.CrossRefGoogle Scholar
Nwaodua, E.C., Ortiz, J.D., & Griffith, E.M. (2014) Diffuse spectral reflectance of surficial sediments indicates sedimentary environments on the shelves of the Bering Sea and western Arctic. Marine Geology, 355, 218233.CrossRefGoogle Scholar
Ody, A., Poulet, F., Quantin, C., Bibring, J.P., Bishop, J.L, & Dyar, M.D. (2015) Candidates source regions of martian meteorites as identified by OMEGA/MEx. Icarus, 258, 366383.CrossRefGoogle Scholar
Orenberg, J. & Handy, J. (1992) Reflectance spectroscopy of palagonite and iron-rich montmorillonite clay mixtures: Implications for the surface composition of Mars. Icarus, 96, 219225.CrossRefGoogle Scholar
Papike, J.J. (1989) Planetary materials. In: Reviews in mineralogy, 36. Mineralogical Society of America, Chantilly, VA.Google Scholar
Parente, M., Makarewicz, H.D., & Bishop, J.L. (2011) Decomposition of mineral absorption bands using nonlinear least squares curve fitting: Application to martian meteorites and CRISM data. Planetary and Space Science, 59, 423442.CrossRefGoogle Scholar
Parfitt, R.L. (2009) Allophane and imogolite: Role in soil biogeochemical processes. Clay Minerals, 44, 135155.CrossRefGoogle Scholar
Petit, S., Madejova, J., Decarreau, A., & Martin, F. (1999) Characterization of octahedral subsitutions in kaolinites using near infrared spectroscopy. Clays and Clay Minerals, 47, 103108.CrossRefGoogle Scholar
Petit, S., Decarreau, A., Martin, F., & Buchet, R. (2004a) Refined relationship between the position of the fundamental OH stretching and the first overtones for clays. Physics and Chemistry of Minerals, 31, 585592.CrossRefGoogle Scholar
Petit, S., Martin, F., Wiewiora, A., de Parseval, P., & Decarreau, A. (2004b) Crystal-chemistry of talc: A near infrared (NIR) spectroscopy study. American Mineralogist, 89, 319326.CrossRefGoogle Scholar
Pieters, C.M. (1983) Strength of mineral absorption features in the transmitted component of near-infrared reflected light: First results from RELAB. Journal of Geophysical Research, 88, 95349544.CrossRefGoogle Scholar
Pieters, C.M. (1996) Plagioclase and maskelynite diagnostic features. 27th Lunar Planet. Sci. Conf., Abstract #1031.
Pieters, C.M. & Hiroi, T. (2004) RELAB (Reflectance Experiment Laboratory): A NASA multiuser spectroscopy facility. 35th Lunar Planet. Sci. Conf., Abstract #1720.
Pieters, C.M. & Mustard, J.F. (1988) Exploration of crustal/mantle material for the Earth and Moon using reflectance spectroscopy. Remote Sensing Environment, 24, 151178.CrossRefGoogle Scholar
Pieters, C.M., Hawke, B.R., Gaffey, M., & McFadden, L.A. (1983) Possible lunar source areas of meteorite ALHA81005: Geochemical remote sensing information. Geophysical Research Letters, 10, 813816.CrossRefGoogle Scholar
Pieters, C.M., Mustard, J.F., Pratt, S.F., Sunshine, J.M., & Hoppin, A. (1993) Visible-infrared properties of controlled laboratory soils. 24th Lunar Planet. Sci. Conf., Abstract, 1147–1148.
Pieters, C.M., Mustard, J.F., & Sunshine, J.M. (1996) Quantitative mineral analyses of planetary surfaces using reflectance spectroscopy. In: Mineral spectroscopy: A tribute to Roger G. Burns (Dyar, M.D., McCammon, C., & Schaefer, M.W., eds.). The Geochemical Society, Houston, TX, 307325.Google Scholar
Pieters, C.M., Klima, R.L., Hiroi, T., et al. (2008) The origin of brown olivine in martian dunite NWA 2737: Integrated spectroscopic analyses of brown olivine. Journal of Geophysical Research, 113, E06004, DOI:10.1029/2007JE002939.CrossRefGoogle Scholar
Post, J.L. (1984) Saponite from near Ballarat, California. Clays and Clay Minerals, 32, 147152.CrossRefGoogle Scholar
Post, J.L. & Noble, P.N. (1993) The near-infrared combination band frequencies of dioctahedral smectites, micas, and illites. Clays and Clay Minerals, 41, 639644.CrossRefGoogle Scholar
Post, J.L., Cupp, B.L., & Madsen, F.T. (1997) Beidellite and associated clays from the DeLamar mine and Florida mountain area, Idaho. Clays and Clay Mineral, 45, 240250.CrossRefGoogle Scholar
Powers, D.A., Rossman, G.R., Schugar, H.J., & Gray, H.B. (1975) Magnetic behavior and infrared spectra of jarosite, basic iron sulfate, and their chromate analogs. Journal of Solid State Chemistry, 13, 113.CrossRefGoogle Scholar
Rice, M.S., Cloutis, E.A., Bell, J.F. III, et al. (2013) Reflectance spectra diversity of silica-rich materials: Sensitivity to environment and implications for detections on Mars. Icarus, 223, 499533.CrossRefGoogle Scholar
Ross, S.D. (1974) Phosphates and Other Oxyanions of Group V. In: The infrared spectra of minerals (Farmer, V.C., ed.). The Mineralogical Society, London, 383422.CrossRefGoogle Scholar
Roush, T.L., Bishop, J.L., Brown, A.J., Blake, D.F., & Bristow, T.F. (2015) Laboratory reflectance spectra of clay minerals mixed with Mars analog materials: Toward enabling quantitative clay abundances from Mars spectra. Icarus, 258, 454466.CrossRefGoogle Scholar
Ruesch, O., Hiesinger, H., Cloutis, E., et al. (2015) Near infrared spectroscopy of HED meteorites: Effects of viewing geometry and compositional variations. Icarus, 258, 384401.CrossRefGoogle Scholar
Salisbury, J.W. & Hunt, G.R. (1974) Meteorite spectra and weathering. Journal of Geophysical Research, 79, 4493–4441.CrossRefGoogle Scholar
Salisbury, J.W., D’Aria, D.M., & Jarosewich, E. (1991) Midinfrared (2.5–13.5 µm) reflectance spectra of powdered stony meteorites. Icarus, 92, 280297.CrossRefGoogle Scholar
Saper, L. & Bishop, J.L. (2011) Reflectance spectroscopy of nontronite and ripidolite mineral mixtures in context of phyllosilicate unit composition at Mawrth Vallis. 42nd Lunar Planet. Sci. Conf., Abstract #2029.
Schade, U. & Wäsch, R. (1999) Near-infrared reflectance spectra from bulk samples of the two martian meteorites Zagami and Nakhla. Meteoritics and Planetary Science, 34, 417424.CrossRefGoogle Scholar
Schade, U., Wäsch, R., & Moroz, L. (2004) Near-infrared reflectance spectroscopy of Ca-rich clinopyroxenes and prospects for remote spectral characterization of planetary surfaces. Icarus, 168, 8092.CrossRefGoogle Scholar
Scheinost, A.C., Chavernas, A., Barrón, V., & Torrent, J. (1998) Use and limitations of second-derivative diffuse reflectance spectroscopy in the visible to near-infrared range to identify and quantify Fe oxide minerals in soils. Clays and Clay Minerals, 46, 528536.CrossRefGoogle Scholar
Sherman, D.M. & Waite, T.D. (1985) Electronic spectra of Fe3+ oxides and oxide hydroxides in the near IR to near UV. American Mineralogist, 70, 12621269.Google Scholar
Sherman, D.M., Burns, R.G., & Burns, V.M. (1982) Spectral characteristics of the iron oxides with application to the martian bright region mineralogy. Journal of Geophysical Research, 87, 1016910180.CrossRefGoogle Scholar
Shkuratov, Y.G. & Grynko, Y.S. (2005) Light scattering by media composed of semitransparent particles of different shapes in ray optics approximation: Consequences for spectroscopy, photometry, and polarimetry of planetary regoliths. Icarus, 173, 1628.CrossRefGoogle Scholar
Singer, R.B. (1981) Near-infrared spectral reflectance of mineral mixtures: Systematic combinations of pyroxenes, olivine, and iron oxides. Journal of Geophysical Research, 86, 79677982.CrossRefGoogle Scholar
Singer, R.B. & Roush, T.L. (1983) Spectral reflectance properties of particulate weathered coatings on rocks: Laboratory modeling and applicability to Mars. 14th Lunar Planet. Sci. Conf., Abstract, 708–709.
Singer, R.B. & Roush, T.L. (1985) Effects of temperature on remotely sensed mineral absorption features. Journal of Geophysical Research, 90, 12,43412,444.CrossRefGoogle Scholar
Song, X. & Boily, J.-F. (2012) Variable hydrogen bond strength in akaganéite. The Journal of Physical Chemistry C, 116, 23032312.CrossRefGoogle Scholar
Song, X. & Boily, J.-F. (2013) Water vapor diffusion into a nanostructured iron oxyhydroxide. Inorganic Chemistry, 52, 71077113.CrossRefGoogle ScholarPubMed
Sugihara, T., Ohtake, M., Owada, A., Ishii, T., Otsuki, M., & Takeda, H. (2004) Petrology and reflectance spectroscopy of lunar meteorite Yamato 981031: Implications for the source region of the meteorite and remote-sensing spectroscopy. Antarctic Meteorite Research, 17, 209230.Google Scholar
Sun, V.Z., Milliken, R.E., & Robertson, K.M. (2016) Hydrated silica on Mars: Relating geologic setting to degree of hydration, crystallinity, and maturity through coupled orbital and laboratory studies. 47th Lunar Planet. Sci. Conf., Abstract #2416.
Sunshine, J.M. & Pieters, C.M. (1993) Estimating modal abundances from the spectra of natural and laboratory pyroxene mixtures using the Modified Gaussian Model. Journal of Geophysical Research, 98, 90759087.CrossRefGoogle Scholar
Sunshine, J.M. & Pieters, C.M. (1998) Determining the composition of olivine from reflectance spectroscopy. Journal of Geophysical Research, 103, 13,67513,688.CrossRefGoogle Scholar
Sunshine, J.M., Pieters, C.M., & Pratt, S.F. (1990) Deconvolution of mineral absorption bands: An improved approach. Journal of Geophysical Research, 95, 69556966.CrossRefGoogle Scholar
Sunshine, J.M., McFadden, L.A., & Pieters, C.M. (1993) Reflectance spectra of the Elephant Moraine A79001 meteorite: Implications for remote sensing of planetary bodies. Icarus, 105, 7991.CrossRefGoogle Scholar
Sunshine, J.M., Bus, S.J., McCoy, T.J., Burbine, T.H., Corrigan, C.M., & Binzel, P. (2004) High-calcium pyroxene as an indicator of igneous differentiation in asteroids and meteorites. Meteoritics and Planetary Science, 39, 13431357.CrossRefGoogle Scholar
Sunshine, J.M., Bus, S.J., Corrigan, C.M., McCoy, T.J., & Burbine, T.H. (2007) Olivine-dominated asteroids and meteorites: Dinstinguishing nebular and igneous histories. Meteoritics and Planetary Science, 42, 155170.CrossRefGoogle Scholar
Swayze, G.A., Lowers, H.A., Benzel, W.M., et al. (2018) Characterizing the source of potentially asbestos-bearing commercial vermiculite insulation using in situ IR spectroscopy. American Mineralogist, 103, 517549.CrossRef
Tarantola, A. & Valette, B. (1982) Generalized nonlinear inverse problems solved using the least squares criterion. Reviews of Geophysics and Space Physics, 20, 219232.CrossRefGoogle Scholar
van Olphen, H. & Fripiat, J.J. (1979) Data handbook for clay materials and other non-metallic minerals. Pergamon Press, Oxford.Google Scholar
Wang, F., Bowen, B.B., Seo, J.-H., & Michalski, G. (2018) Laboratory and field characterization of visible to near-infrared spectral reflectance of nitrate minerals from the Atacama Desert, Chile, and implications for Mars. American Mineralogist, 103, 197206.CrossRefGoogle Scholar
Wasson, J.T. (1985) Meteorites: Their record of early Solar System history. W.H. Freeman, New York.Google Scholar
Weir, C.E. & Lippincott, E.R. (1961) Infrared studies of aragonite, calcite, and vaterite type structures in the borates, carbonates, and nitrates. Journal of Research of the National Bureau of Standards A: Physics and Chemistry, 65A, 173183.CrossRefGoogle Scholar

References

Allamandola, L.J., Sandford, S.A., & Wopenka, B. (1987) Interstellar polycyclic aromatic hydrocarbons and carbon in interplanetary dust particles and meteorites. Science, 237, 5659.CrossRefGoogle Scholar
Altwegg, K., Balsiger, H., Berthelier, J.J., et al. (2017) Organics in comet 67P – a first comparative analysis of mass spectra from ROSINA-DFMS, COSAC, and Ptolemy. Monthly Notices of the Royal Astronomical Society, 469, Issue Supplement 2, S130–S141.CrossRefGoogle Scholar
Barucci, M.A., Merlin, F., Guilbert, A., et al. (2008) Surface composition and temperature of the TNO Orcus. Astronomy & Astrophysics, 479, L13L16.CrossRefGoogle Scholar
Barucci, M.A., Dalle Ore, C.M., Perna, D., et al. (2015) (50000) Quaoar: Surface composition variability. Astronomy & Astrophysics, 584, A107.CrossRefGoogle Scholar
Bennett, C.J., Pirim, C., & Orlando, T.M. (2013) Space-weathering of Solar System bodies: A laboratory perspective. Chemical Reviews, 113, 90869150.CrossRefGoogle ScholarPubMed
Blake, D., Allamandola, L., Sandford, S., Hudgins, D., & Freund, F. (1991) Clathrate hydrate formation in amorphous cometary ice analogs in vacuo. Science, 254, 548551.CrossRefGoogle ScholarPubMed
Brown, A.J. (2014) Spectral bluing induced by small particles under the Mie and Rayleigh regimes. Icarus, 239, 8595.CrossRefGoogle Scholar
Brown, A.J., Calvin, W.M., Becerra, P., & Byrne, S. (2016) Martian north polar cap summer water cycle. Icarus, 277, 401415.CrossRefGoogle Scholar
Brown, M.E. & Calvin, W.M. (2000) Evidence for crystalline water and ammonia ices on Pluto’s satellite Charon. Science, 287, 107109.CrossRefGoogle ScholarPubMed
Cable, M.L., Hörst, S.M., Hodyss, R., et al. (2012) Titan tholins: Simulating Titan organic chemistry in the Cassini-Huygens era. Chemical Reviews, 112, 18821909.CrossRefGoogle ScholarPubMed
Capaccioni, F., Coradini, A., Filacchione, G., et al. (2015) The organic-rich surface of comet 67P/Churyumov-Gerasimenko as seen by VIRTIS/Rosetta. Science, 347, aaa0628.CrossRefGoogle ScholarPubMed
Chaban, G.M., Bernstein, M., & Cruikshank, D.P. (2007) Carbon dioxide on planetary bodies: Theoretical and experimental studies of molecular complexes. Icarus, 187, 592599.CrossRefGoogle Scholar
Chassefière, E., Dartois, E., Herri, J.-M., et al. (2013) CO2–SO2 clathrate hydrate formation on early Mars. Icarus, 223, 878891.CrossRefGoogle Scholar
Choukroun, M., Kieffer, S.W., Lu, X., & Tobie, G. (2013) Clathrate hydrates: Implications for exchange processes in the outer Solar System. In: The science of Solar System ices (Gudipati, M.S. & Castillo-Rogez, J., eds.). Springer Science+Business Media, New York, 409454.CrossRefGoogle Scholar
Clark, R.N. (1981) The spectral reflectance of water‐mineral mixtures at low temperatures. Journal of Geophysical Research, 86, 30743086.CrossRefGoogle Scholar
Clark, R.N. & Lucey, P.G. (1984) Spectral properties of ice‐particulate mixtures and implications for remote sensing: 1. Intimate mixtures. Journal of Geophysical Research, 89, 63416348.CrossRefGoogle Scholar
Clark, R.N. & Roush, T.L. (1984) Reflectance spectroscopy: Quantitative analysis techniques for remote sensing applications. Journal of Geophysical Research, 89, 63296340.CrossRefGoogle Scholar
Clark, R.N., Fanale, F.P., & Gaffey, M.J. (1986) Surface composition of satellites. In: Satellites (Burns, J. & Matthews, M.S., eds.), University of Arizona Press, Tucson, 437491.Google Scholar
Clark, R.N., Curchin, J.M., Hoefen, T.M., & Swayze, G.A. (2009) Reflectance spectroscopy of organic compounds: 1. Alkanes. Journal of Geophysical Research, 114, E03001, DOI:10.1029/2008JE003150.CrossRefGoogle Scholar
Clark, R.N., Cruikshank, D.P., Jaumann, R., et al. (2012) The surface composition of Iapetus: Mapping results from Cassini VIMS. Icarus, 218, 831860.CrossRefGoogle Scholar
Clark, R.N., Carlson, R., Grundy, W., & Noll, K. (2013) Observed ices in the Solar System. In: The science of Solar System ices (Gudipati, M.S. & Castillo-Rogez, J., eds.). Springer Science+Business Media, New York, 346.CrossRefGoogle Scholar
Clark, R.N., Swayze, G.A., Carlson, R., Grundy, W., & Noll, K. (2014) Spectroscopy from space. In: Spectroscopic methods in mineralogy and material sciences (Henderson, G., ed.). Reviews in Mineralogy & Geochemistry, 78, 399446.Google Scholar
Clemett, S.J., Maechling, C.R., Zare, R.N., Swan, P.D., & Walker, R.M. (1993) Identification of complex aromatic molecules in individual interplanetary dust particles. Science, 262, 721725.CrossRefGoogle ScholarPubMed
Cloutis, E.A. (1989) Spectral reflectance properties of hydrocarbons: Remote-sensing implications. Science, 245, 165168.CrossRefGoogle ScholarPubMed
Cloutis, E.A. (2003) Quantitative characterization of coal properties using bidirectional diffuse reflectance spectroscopy. Fuel, 82, 22392254.CrossRefGoogle Scholar
Cloutis, E.A., Gaffey, M.J., & Moslow, T.F. (1994) Spectral reflectance properties of carbon-bearing materials. Icarus, 107, 276287.CrossRefGoogle Scholar
Cloutis, E.A., Hiroi, T., Gaffey, M.J., Alexander, C.M.O.D., & Mann, P. (2011) Spectral reflectance properties of carbonaceous chondrites: 1. CI chondrites. Icarus, 212, 180209.CrossRefGoogle Scholar
Cook, J.C., Desch, S.J., Roush, T.L., Trujillo, C.A., & Geballe, T. (2007) Near-infrared spectroscopy of Charon: Possible evidence for cryovolcanism on Kuiper Belt objects. The Astrophysical Journal, 663, 1406.CrossRefGoogle Scholar
Cooper, J.F., Christian, E.R., Richardson, J.D., & Wang, C. (2003) Proton irradiation of Centaur, Kuiper Belt, and Oort Cloud objects at plasma to cosmic ray energy. Earth, Moon, and Planets, 92, 961–277.CrossRefGoogle Scholar
Cronin, J.R., Pizzarello, S., & Cruikshank, D.P. (1988) Organic matter in carbonaceous chondrites, planetary satellites, asteroids and comets. In: Meteorites and the early Solar System (Kerridge, J.F. & Matthews, M.S., eds.). University of Arizona Press, Tucson, 819857.Google Scholar
Cruikshank, D. & Khare, B. (2000) Planetary surfaces of low albedo: Organic material throughout the Solar System. A new era in bioastronomy (Lemarchand, G.A. & Meech, K.J., eds.) ASP Conference Series, 213, 253262.Google Scholar
Cruikshank, D.P., Brown, R., & Clark, R. (1985) Methane ice on Triton and Pluto. In: Ices in the Solar System (Klinger, J., Benest, D., Dollfus, A., & Smoluchowski, R., eds.). Springer-Verlag, New York, 817827.CrossRefGoogle Scholar
Cruikshank, D.P., Roush, T.L., Owen, T.C., et al. (1993) Ices on the surface of Triton. Science, 261, 742745.CrossRefGoogle ScholarPubMed
Cruikshank, D., Roush, T., Bartholomew, M., et al. (1998) The composition of centaur 5145 Pholus. Icarus, 135, 389407.CrossRefGoogle Scholar
Cruikshank, D.P., Meyer, A.W., Brown, R.H., et al. (2010) Carbon dioxide on the satellites of Saturn: Results from the Cassini VIMS investigation and revisions to the VIMS wavelength scale. Icarus, 206, 561572.CrossRefGoogle Scholar
Cull, S., Arvidson, R.E., Mellon, M., et al. (2010) Seasonal H2O and CO2 ice cycles at the Mars Phoenix landing site: 1. Prelanding CRISM and HiRISE observations. Journal of Geophysical Research, 115, DOI:10.1029/2009JE003340.Google Scholar
Cuzzi, J., Clark, R., Filacchione, G., et al. (2009) Ring particle composition and size distribution. In: Saturn after Cassini/Huygens (Dougherty, M.K., Esposito, L.W., & Krimigis, S.M., eds.). Springer Science+Business Media, New York, 459509.Google Scholar
Dalle Ore, C.M., Barucci, M., Emery, J., et al. (2015) The composition of “ultra-red” TNOS and Centaurs. Icarus, 252, 311326.CrossRefGoogle Scholar
Dalle Ore, C. M., Protopapa, S., Cook, J.C. et al. (2018) Ices on Charon: Distribution of H2O and NH3 from New Horizons LEISA observations. Icarus, 300, 2132.CrossRefGoogle Scholar
Dartois, E. (2010) Clathrates hydrates FTIR spectroscopy: Infrared signatures and their astrophysical significance. Molecular Physics, 108, 22732278.CrossRefGoogle Scholar
Dartois, E. & Deboffle, D. (2008) Methane clathrate hydrate FTIR spectrum: Implications for its cometary and planetary detection. Astronomy & Astrophysics, 490, L19-L22.CrossRefGoogle Scholar
Dartois, E. & Schmitt, B. (2009) Carbon dioxide clathrate hydrate FTIR spectrum-near infrared combination modes for astrophysical remote detection. Astronomy & Astrophysics, 504, 869873.CrossRefGoogle Scholar
Dartois, E., Engrand, C., Brunetto, R., et al. (2013) UltraCarbonaceous Antarctic micrometeorites, probing the Solar System beyond the nitrogen snow-line. Icarus, 224, 243252.CrossRefGoogle Scholar
de Bergh, C., Schmitt, B., Moroz, L., Quirico, E., & Cruikshank, D.P. (2008) Laboratory data on ices, refractory carbonaceous materials, and minerals relevant to transneptunian objects and Centaurs. In: The Solar System beyond Neptune (Barucci, A., Boehnhardt, H., Cruikshank, D.P., & Morbidelli, A., eds.). University of Arizona Press, Tucson, 483506.Google Scholar
Devlin, J.P. & Buch, V. (1997) Vibrational spectroscopy and modeling of the surface and subsurface of ice and of ice-adsorbate interactions. Journal of Physical Chemistry B, 101, 60956098.CrossRefGoogle Scholar
Devlin, J.P. & Buch, V. (2003) Ice nanoparticles and ice adsorbate interactions: FTIR spectroscopy and computer simulations. In: Water in confining geometries (Buch, V. & Devlin, J.P., eds.). Springer Science+Business Media, 425462.CrossRefGoogle Scholar
Flynn, G., Keller, L., Feser, M., Wirick, S., & Jacobsen, C. (2003) The origin of organic matter in the Solar System: Evidence from the interplanetary dust particles. Geochimica et Cosmochimica Acta, 67, 47914806.CrossRefGoogle Scholar