Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-10T10:16:07.222Z Has data issue: false hasContentIssue false

18 - Compositional Analysis of the Moon in the Visible and Near-Infrared Regions

from Part IV - Applications to Planetary Surfaces

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
Get access

Summary

Advanced spectroscopic sensors recently flown to the Moon have revealed unexpected discoveries about Earth’s nearest neighbor as well as provided detailed insights and constraints about how early crust evolves on an airless planetary body. Discussed here are (a) global assessment of the variety and distribution of major lunar mineral components and lithologies; (b) some of the remarkable new findings, such as the pervasive presence of OH across the surface and new rock types identified (Mg-spinel anorthosite) that are not identified in current lunar samples; and (c) expectations for the future as additional modern sensors provide a stronger foundation for remote compositional analysis of the Moon. Spectroscopic data continue to provide the cornerstone for identifying and understanding the regional and global character of lunar compositional variations and document key products and processes of crustal evolution.

Type
Chapter
Information
Remote Compositional Analysis
Techniques for Understanding Spectroscopy, Mineralogy, and Geochemistry of Planetary Surfaces
, pp. 368 - 392
Publisher: Cambridge University Press
Print publication year: 2019

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Adams, J. & McCord, T. (1970) Remote sensing of lunar surface mineralogy: Implications from visible and near-infrared reflectivity of Apollo 11 samples. Geochimica et Cosmochimica Acta Supplement, 1, 1937.Google Scholar
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. & Jones, R.L. (1970) Spectral reflectivity of lunar samples. Science, 167, 737739.Google Scholar
Adams, J.B., Pieters, C., & McCord, T.B. (1974) Orange glass: Evidence for regional deposits of pyroclastic origin on the moon. Proceedings of the 5th Lunar Planet. Sci. Conf., 171186.Google Scholar
Bandfield, J.L., Poston, M.J., Klima, R.L., & Edwards, C.S. (2018) Widespread distribution of OH/H2O on the lunar surface inferred from spectral data. Nature Geoscience, 11(3), 173177.Google Scholar
Bell, P., Mao, H., & Weeks, R. (1976) Optical spectra and electron paramagnetic resonance of lunar and synthetic glasses: A study of the effects of controlled atmosphere, composition, and temperature. Proceedings of the Lunar Planet. Sci. Conf., 25432559.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.Google Scholar
Bender, H.A., Mouroulis, P., Smith, C.D., et al. (2015) Snow and water imaging spectrometer (SWIS): Optomechanical and system design for a CubeSat-compatible instrument. In: Imaging Spectrometry XX (Pagano, T.S. & Silny, J.F, eds.). SPIE Proceedings, 9611.Google Scholar
Besse, S., Sunshine, J., & Gaddis, L. (2014) Volcanic glass signatures in spectroscopic survey of newly proposed lunar pyroclastic deposits. Journal of Geophysical Research, 119, 355372.CrossRefGoogle Scholar
Bhattacharya, S., Saran, S., Dagar, A., et al. (2013) Endogenic water on the Moon associated with non-mare silicic volcanism: Implications for hydrated lunar interior. Current Science, 105, 685691.Google Scholar
Blewett, D.T., Coman, E.I., Hawke, B.R., Gillis-Davis, J.J., Purucker, M.E., & Hughes, C.G. (2011) Lunar swirls: Examining crustal magnetic anomalies and space weathering trends. Journal of Geophysical Research, 116, E02002, DOI:10.1029/2010JE003656.Google Scholar
Boardman, J.W., Pieters, C.M., Green, R.O., et al. (2011) Measuring moonlight: An overview of the spatial properties, lunar coverage, selenolocation, and related Level 1B products of the Moon Mineralogy Mapper. Journal of Geophysical Research, 116, E00G14, DOI:10.1029/2010JE003730.Google Scholar
Boyd, A.K., Robinson, M.S., & Sato, H. (2012) Lunar Reconnaissance Orbiter wide angle camera photometry: An empirical solution. 43rd Lunar Planet. Sci. Conf., Abstract # 2795.Google Scholar
Burns, R.G. (1993) Mineralogical applications of crystal field theory. Cambridge University Press, Cambridge.CrossRefGoogle Scholar
Cahill, J.T., Lucey, P.G., Gillis, J.J., & Steutel, D. (2004) Verification of quality and compatibility for the newly calibrated Clementine NIR data set. 35th Lunar Planet. Sci., Abstract #1469.Google Scholar
Charette, M.P., McCord, T.B., Pieters, C., & Adams, J.B. (1974) Application of remote spectral reflectance measurements to lunar geology classification and determination of titanium content of lunar soils. Journal of Geophysical Research, 79, 16051613.CrossRefGoogle Scholar
Cheek, L., Pieters, C.M., Parman, S., Dyar, M.D., Speicher, E.A., & Cooper, R.F. (2011a) Spectral characteristics of plagioclase with variable iron content: Applications to remote sensing of the lunar crust. 42nd Lunar Planet. Sci. Conf., Abstract #1617.Google Scholar
Cheek, L.C. & Pieters, C.M. (2014) Reflectance spectroscopy of plagioclase-dominated mineral mixtures: Implications for characterizing lunar anorthosites remotely. American Mineralogist, 99, 18711892.Google Scholar
Cheek, L.C., Pieters, C.M., Boardman, J.W., et al. (2011) Goldschmidt crater and the Moon’s north polar region: Results from the Moon Mineralogy Mapper (M3). Journal of Geophysical Research, 116, E00G02, DOI:10.1029/2010je003702.Google Scholar
Cheek, L.C., Donaldson, H.K.L., Pieters, C.M., Head, J.W., & Whitten, J.L. (2013) The distribution and purity of anorthosite across the Orientale Basin: New perspectives from Moon Mineralogy Mapper data. Journal of Geophysical Research, 118, 18051820.Google Scholar
Clark, R.N. (1979) Planetary reflectance measurements in the region of planetary thermal emission. Icarus, 40, 94103.CrossRefGoogle Scholar
Clark, R.N. (2009) Detection of adsorbed water and hydroxyl on the Moon. Science, 326, 562564.CrossRefGoogle ScholarPubMed
Clark, R.N., Pieters, C.M., Green, R.O., Boardman, J.W., & Petro, N.E. (2011) Thermal removal from near-infrared imaging spectroscopy data of the Moon. Journal of Geophysical Research, 116, E00G16, DOI:10.1029/2010JE003751.CrossRefGoogle Scholar
Cloutis, E.A. & Gaffey, M.J. (1991) Spectral-compositional variations in the constituent minerals of mafic and ultramafic assemblages and remote sensing implications. Earth, Moon, and Planets, 53, 1153.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.Google Scholar
Conel, J.E. & Nash, D.B. (1970) Spectral reflectance and albedo of Apollo 11 lunar samples: Effects of irradiation and vitrification and comparison with telescopic observations. Apollo 11 Lunar Sci. Conf., 2013–2023.Google Scholar
Crites, S.T., Lucey, P.G., & Taylor, G.J. (2015) The mafic component of the lunar crust: Constraints on the crustal abundance of mantle and intrusive rock, and the mineralogy of lunar anorthosites. American Mineralogist, 100, 17081716.Google Scholar
Denevi, B.W., Robinson, M.S., Boyd, A.K., Sato, H., Hapke, B.W., & Hawke, B.R. (2014) Characterization of space weathering from Lunar Reconnaissance Orbiter Camera ultraviolet observations of the Moon. Journal of Geophysical Research, 119, 976997.Google Scholar
Dhingra, D., Pieters, C.M., & Head, J.W. (2015) Multiple origins for olivine at Copernicus crater. Earth and Planetary Science Letters, 420, 95101.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
Dyar, M.D., Hibbitts, C.A., & Orlando, T.M. (2010) Mechanisms for incorporation of hydrogen in and on terrestrial planetary surfaces. Icarus, 208, 425437.Google Scholar
Eliason, E., Isbell, C., Lee, E., et al. (1999) Mission to the Moon: The Clementine UVVIS Global Mosaic. PDS CL_4001–4078. www.lpi.usra.edu/lunar/tools/clementine/instructions/UVVIS_DIM_Info.htmlGoogle Scholar
Eliason, E.M., Lee, E.M., Becker, T.L., et al. (2003) A near-infrared (NIR) global multispectral map of the Moon from Clementine. 34th Lunar Planet. Sci. Conf., Abstract #2093.Google Scholar
Feldman, W.C., Maurice, S., Binder, A.B., Barraclough, B.L., Elphic, R.C., & Lawrence, D.J. (1998) Fluxes of fast and epithermal neutrons from lunar Prospector: Evidence for water ice at the lunar poles. Science, 281, 14961500.Google Scholar
Gaddis, L.R., Staid, M.I., Tyburczy, J.A., Hawke, B.R., & Petro, N.E. (2003) Compositional analyses of lunar pyroclastic deposits. Icarus, 161, 262280.Google Scholar
Giguere, T.A., Taylor, G.J., Hawke, B.R., & Lucey, P.G. (2000) The titanium contents of lunar mare basalts. Meteoritics and Planetary Science, 35, 193200.CrossRefGoogle Scholar
Green, R. (2016) 30 years of thermally controlled imaging spectrometers for Earth and planetary science. 46th International Conference on Environmental Systems.Google Scholar
Green, R., Pieters, C.M., Mouroulis, P., et al. (2011) The Moon Mineralogy Mapper (M3) imaging spectrometer for lunar science: Instrument description, calibration, on-orbit measurements, science data calibration and on-orbit validation. Journal of Geophysical Research, 116, E00G19, DOI:10.1029/2011JE003797.CrossRefGoogle Scholar
Hapke, B. (2001) Space weathering from Mercury to the asteroid belt. Journal of Geophysical Research, 106, 1003910073.CrossRefGoogle Scholar
Hawke, B.R., Peterson, C.A., Blewett, D.T., et al. (2003) Distribution and modes of occurrence of lunar anorthosite. Journal of Geophysical Research, 108, 5050, DOI:10.1029/2002JE001890.Google Scholar
Hazen, R.M., Bell, P.M., & Mao, H.K. (1978) Effects of compositional variation on absorption spectra of lunar pyroxenes. Proceedings of the 9th Lunar Planet. Sci. Conf., 29192934.Google Scholar
Heiken, G., Vaniman, D., & French, B.M. (1991) Lunar sourcebook: A user’s guide to the Moon. Cambridge University Press, New York.Google Scholar
Hiroi, T., Pieters, C., & Morris, R. (1997) New considerations for estimating lunar soil maturity from VIS-NIR reflectance spectroscopy. 28th Lunar Planet. Sci. Conf., Abstract #1152.Google Scholar
Hook, S.J., Johnson, W.R., & Abrams, M.J. (2013) NASA’s Hyperspectral Thermal Emission Spectrometer (HyTES). In: Thermal infrared remote sensing: Sensors, methods, applications (Kuenzer, C. & Dech, S., eds.). Springer, Dordrecht, 93115.Google Scholar
Isaacson, P.J. & Pieters, C.M. (2009) Northern Imbrium noritic anomaly. Journal of Geophysical Research, 114, E09007, DOI:10.1029/2008JE003293.Google Scholar
Isaacson, P.J., Sarbadhikari, A.B., Pieters, C.M., et al. (2011a) The lunar rock and mineral characterization consortium: Deconstruction and integrated mineralogical, petrologic, and spectroscopic analyses of mare basalts. Meteoritics and Planetary Science, 46, 228251.Google Scholar
Isaacson, P.J., Pieters, C.M., Besse, S., et al. (2011b) Remote compositional analysis of lunar olivine rich lithologies with Moon Mineralogy Mapper (M3) spectra. Journal of Geophysical Research, 116, E00G11, DOI:10.1029/2010JE003731.Google Scholar
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.Google Scholar
Jolliff, B.I., Wieczorek, M.A., Shearer, C.K., & Neal, C.R. (2006) New views of the Moon. Reviews in Mineralogy and Geochemistry, 60. Geochemical Society.Google Scholar
Jolliff, B.L., Wiseman, S.A., Lawrence, S.J., et al. (2011) Non-mare silicic volcanism on the lunar farside at Compton–Belkovich. Nature Geoscience, 4, 566–571.Google Scholar
Keller, L. & Zhang, S. (2015) Rates of space weathering in lunar soils. Space Weathering of Airless Bodies: An Integration of Remote Sensing Data, Laboratory Experiments and Sample Analysis Workshop, Abstract #2056.Google Scholar
Keller, L., Berger, E., Christoffersen, R., & Zhang, S. (2016) Direct determination of the space weathering rates in lunar soils and Itokawa regolith from sample analyses. 47th Lunar Planet. Sci. Conf., Abstract #2525.Google Scholar
Keller, L.P. & McKay, D.S. (1993) Discovery of vapor deposits in the lunar regolith. Science, 261, 13051307.Google Scholar
Keller, L.P. & McKay, D.S. (1997) The nature and origin of rims on lunar soil grains. Geochimica et Cosmochimica Acta, 61, 23312341.CrossRefGoogle Scholar
Klima, R., Cahill, J., Hagerty, J., & Lawrence, D. (2013) Remote detection of magmatic water in Bullialdus crater on the Moon. Nature Geoscience, 6, 737–741.Google Scholar
Klima, R., Buczkowski, D., Ernst, C., & Greenhagen, B. (2017) Geological and spectral analysis of low-calcium pyroxenes around the Imbrium Basin on the Moon. 48th Lunar Planet. Sci. Conf., Abstract #2502.Google Scholar
Klima, R.L. & Petro, N.E. (2017) Remotely distinguishing and mapping endogenic water on the Moon. Philosophical Transactions of the Royal Society A, 375, 20150391.Google 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.Google Scholar
Klima, R.L., Dyar, M.D., & Pieters, C.M. (2011a) Near-infrared spectra of clinopyroxenes: Effects of calcium content and crystal structure. Meteoritics and Planetary Science, 46, 379395.CrossRefGoogle Scholar
Klima, R.L., Pieters, C.M., Boardman, J.W., et al. (2011b) New insights into lunar petrology: Distribution and composition of prominent low Ca pyroxene exposures as observed by the Moon Mineralogy Mapper (M3). Journal of Geophysical Research, 116, DOI:10.1029/2010JE003719.Google Scholar
Kramer, G.Y., Besse, S., Dhingra, D., et al. (2011a) M3 spectral analysis of lunar swirls and the link between optical maturation and surface hydroxyl formation at magnetic anomalies. Journal of Geophysical Research, 116, E00G18, DOI:10.1029/2010JE003729.Google Scholar
Kramer, G.Y., Besse, S., Nettles, J., et al. (2011b) Newer views of the Moon: Comparing spectra from Clementine and the Moon Mineralogy Mapper. Journal of Geophysical Research, 116, E00G04, DOI:10.1029/2010JE003728.Google Scholar
Kramer, G.Y., Kring, D.A., Nahm, A.L., & Pieters, C.M. (2013) Spectral and photogeologic mapping of Schrödinger Basin and implications for post-South Pole-Aitken impact deep subsurface stratigraphy. Icarus, 223, 131148.Google Scholar
Li, S. & Milliken, R.E. (2016a) An empirical thermal correction model for Moon Mineralogy Mapper data constrained by laboratory spectra and Diviner temperatures. Journal of Geophysical Research, 121, 20812107.Google Scholar
Li, S. & Milliken, R.E. (2016b) Heterogeneous water content in the lunar interior: Insights from orbital detection of water in pyroclastic deposits and silicic domes. 47th Lunar Planet. Sci. Conf., Abstract #1568.Google Scholar
Li, S. & Milliken, R.E. (2017) Water on the surface of the Moon as seen by the Moon Mineralogy Mapper: Distribution, abundance, and origins. Science Advances, 3, e1701471.Google Scholar
Lucey, P.G. (2004) Planets-L08701. Mineral maps of the Moon. Geophysical Research Letters, 31, L08701, DOI:10.1029/2003GL019406.CrossRefGoogle Scholar
Lucey, P.G., Blewett, D.T., & Hawke, B.R. (1998) Mapping the FeO and TiO2 content of the lunar surface with multispectral imagery. Journal of Geophysical Research, 103, 36793699.Google Scholar
Lucey, P.G., Blewett, D.T., Eliason, E.M., et al. (2000) Optimized calibration constants for the Clementine NIR camera. 31st Lunar Planet. Sci. Conf., Abstract #1273.Google Scholar
Lucey, P.G., Norman, J.A., Crites, S.T., et al. (2014) A large spectral survey of small lunar craters: Implications for the composition of the lunar mantle. American Mineralogist, 99, 22512257.CrossRefGoogle Scholar
Lundeen, S., McLaughlin, S., & Alanis, R. (2011) Moon Mineralogy Mapper Data Product software interface specification. PDS document Version 9.10. Jet Propulsion Laboratory, JPL D-39032, Pasadena, CA.Google Scholar
McCord, T.B. & Johnson, T.V. (1970) Lunar spectral reflectivity (0.30 to 2.50 microns) and implications for remote mineralogical analysis. Science, 169, 855858.Google Scholar
McCord, T.B., Clark, R.N., Hawke, B.R., et al. (1981) Moon: Near-infrared spectral reflectance, a first good look. Journal of Geophysical Research, 86, 1088310892.Google Scholar
McCord, T.B., Taylor, L.A., Combe, J.P., et al. (2011) Sources and physical processes responsible for OH/H2O in the lunar soil as revealed by the Moon Mineralogy Mapper (M3). Journal of Geophysical Research, 116, E00G05, DOI:10.1029/2010JE003711.Google Scholar
McEwen, A.S. & Robinson, M. (1997) Mapping of the Moon by Clementine. Advances in Space Research, 19(10), 15231533.Google Scholar
McEwen, A.S., Eliason, E., Lucey, P., et al. (1998) Summary of radiometric calibration and photometric normalization steps for the Clementine UVVIS images. 29th Lunar Planet. Sci. Conf., Abstract 1466–1467.Google Scholar
Milliken, R.E. & Li, S. (2017) Remote detection of widespread indigenous water in lunar pyroclastic deposits. Nature Geoscience, 10, 561–565.Google Scholar
Moriarty III, D.P. & Pieters, C.M. (2016a) South Pole–Aitken Basin as a probe to the lunar interior. 47th Lunar Planet. Sci. Conf., Abstract #1763.Google Scholar
Moriarty III, D.P. & Pieters, C.M. (2016b) Complexities in pyroxene compositions derived from absorption band centers: Examples from Apollo samples, HED meteorites, synthetic pure pyroxenes, and remote sensing data. Meteoritics and Planetary Science, 51, 207234.CrossRefGoogle Scholar
Moriarty III, D.P. & Pieters, C.M. (2018) The character of South Pole-Aitken Basin: Patterns of surface and subsurface composition. Journal of Geophysical Research, 123, 729747.Google Scholar
Mouroulis, P., Green, R.O., & Chrien, T.G. (2000) Design of pushbroom imaging spectrometers for optimum recovery of spectroscopic and spatial information. Applied Optics, 39, 22102220.Google Scholar
Nakamura, R., Yamamoto, S., Matsunaga, T., et al. (2012) Compositional evidence for an impact origin of the Moon’s Procellarum basin. Nature Geoscience, 5(11),775778, DOI:10.1038/ngeo1614.Google Scholar
National Research Council, Space Studies Board. (2007) Scientific context for exploration of the Moon. National Academies Press, Washington, DC.Google Scholar
Noble, S.K., Pieters, C.M., Hiroi, T., & Taylor, L.A. (2006) Using the modified Gaussian model to extract quantitative data from lunar soils. Journal of Geophysical Research, 111, DOI:10.1029/2006JE002721.Google Scholar
Noble, S.K., Pieters, C.M., & Keller, L.P. (2007) An experimental approach to understanding the optical effects of space weathering. Icarus, 192, 629642.Google Scholar
Nozette, S., Rustan, P., Pleasance, L.P., et al. (1994) The Clementine Mission to the Moon: Scientific overview. Science, 266, 18351839.Google Scholar
Ohtake, M., Matsunaga, T., Haruyama, J., et al. (2009) The global distribution of pure anorthosite on the Moon. Nature, 461, 236240.Google Scholar
Ohtake, M., Matsunaga, T., Yokota, Y., et al. (2010) Deriving the absolute reflectance of lunar surface using SELENE (Kaguya) multiband imager data. Space Science Reviews, 154, 5777.Google Scholar
Ohtake, M., Pieters, C., Isaacson, P., et al. (2013) One Moon, many measurements 3: Spectral reflectance. Icarus, 226, 364374.Google Scholar
Petro, N.E., Isaacson, P.J., Pieters, C.M., Jolliff, B.L., Carter, L.M., & Klima, R.L. (2013) Presence of OH/H2O associated with the lunar Compton-Belkovich volcanic complex identified by the Moon Mineralogy Mapper (M3). 44th Lunar Planet. Sci. Conf., 2688.Google Scholar
Pieters, C.M. (1978) Mare basalt types on the front side of the moon: A summary of spectral reflectance data. Proceedings of the 9th Lunar Sci. Conf. (Suppl. 10, Geochimica et Cosmochimica Acta), 28252849.Google Scholar
Pieters, C.M. (1982) Copernicus crater central peak: Lunar mountain of unique composition. Science, 215, 5961.Google Scholar
Pieters, C.M. (1993) Compositional diversity and stratigraphy of the Lunar crust derived from reflectance spectroscopy. In: Remote geochemical analysis: Elemental and mineralogical composition (Pieters, C. & Englert, P., eds.). Cambridge University Press, Cambridge, 309339.Google Scholar
Pieters, C.M. (1996) Plagioclase and maskelynite diagnostic features. 27th Lunar Planet. Science Conf., Abstract #1031.Google Scholar
Pieters, C.M. (2017) Origin and importance of “featureless” plagioclase on the Moon. 5th Eur. Lunar Symp., Munster, Germany.Google Scholar
Pieters, C.M. & Garrick-Bethell, I. (2015) Hydration variations at lunar swirls. 46th Lunar Planet. Sci. Conf., Abstract #2120.Google Scholar
Pieters, C.M. & Noble, S.K. (2016) Space weathering on airless bodies. Journal of Geophysical Research, 121, 18651884.Google Scholar
Pieters, C.M. & Taylor, L.A. (2003) Systematic global mixing and melting in lunar soil evolution. Geophysical Research Letters, 30, 2048, DOI:10.1029/2003GL018212.Google Scholar
Pieters, C.M., Head, J.W., Adams, J.B., McCord, T.B., Zisk, S.H., & Whitford Stark, J.L. (1980) Late high titanium basalts of the western maria: Geology of the Flamsteed region of Oceanus Procellarum. Journal of Geophysical Research, 85, 39133938.Google Scholar
Pieters, C.M., Taylor, L.A., Noble, S.K., et al. (2000) Space weathering on airless bodies: Resolving a mystery with lunar samples. Meteoritics and Planetary Science, 35, 11011107.Google Scholar
Pieters, C.M., Head III, J.W., Gaddis, L.R., Jolliff, B.L., & Duke, M. (2001) Rock types of South Pole-Aitken Basin and extent of basaltic volcanism. Journal of Geophysical Research, 106, 28,00128,022.Google Scholar
Pieters, C.M., Boardman, J., Buratti, B., et al. (2009a) Mineralogy of the lunar crust in spatial context: First results from the Moon Mineralogy Mapper (M3). 40th Lunar Planet. Sci. Conf., Abstract #2052.Google Scholar
Pieters, C.M., Goswami, J.N., Clark, R., et al. (2009b) Character and spatial distribution of OH/H2O on the surface of the Moon seen by M3 on Chandrayaan-1. Science, 326, 568572.Google Scholar
Pieters, C.M., Besse, S., & Boardman, J. (2011) Mg spinel lithology: A new rock type on the lunar farside. Journal of Geophysical Research, 116, E00G08, DOI:10.1029/2010JE003727.Google Scholar
Pieters, C.M., Boardman, J.W., Ohtake, M., et al. (2013) One Moon, many measurements 1: Radiance values. Icarus, 226, 951963.Google Scholar
Pieters, C.M., Hanna, K.D., Cheek, L., et al. (2014) The distribution of Mg-spinel across the Moon and constraints on crustal origin. American Mineralogist, 99, 18931910.Google Scholar
Prissel, T., Parman, S., Jackson, C., et al. (2014) Pink Moon: The petrogenesis of pink spinel anorthosites and implications concerning Mg-suite magmatism. Earth and Planetary Science Letters, 403, 144156.Google Scholar
Robinson, M., Brylow, S., Tschimmel, M., et al. (2010) Lunar Reconnaissance Orbiter Camera (LROC) instrument overview. Space Science Reviews, 150, 81124.Google Scholar
Sasaki, S., Nakamura, K., Hamabe, Y., Kurahashi, E., & Hiroi, T. (2001) Production of iron nanoparticles by laser irradiation in a simulation of lunar-like space weathering. Nature, 410, 555557.CrossRefGoogle Scholar
Staid, M.I. & Pieters, C.M. (2001) Mineralogy of the last lunar basalts: Results from Clementine. Journal of Geophysical Research, 106, 2788727900.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.Google Scholar
Stöffler, D. (1972) Deformation and transformation of rock-forming minerals by natural and experimental shock processes. 1.Behavior of minerals under shock compression. Fortschritte der Mineralogie, 49, 50113.Google Scholar
Stöffler, D. (1974) Deformation and transformation of rock-forming minerals by natural and experimental shock processes: II. Physical properties of shocked minerals. Fortschritte der Mineralogie, 51, 256289.Google Scholar
Sun, Y.S. & Li, L.L. (2015) Characterization of lunar crust mineralogy with M3 data. 46th Lunar Planet. Sci. Conf., Abstract #2941.Google Scholar
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., Farnham, T.L., Feaga, L.M., et al. (2009) Temporal and spatial variability of lunar hydration as observed by the Deep Impact spacecraft. Science, 326, 565568.CrossRefGoogle ScholarPubMed
Taylor, L.A., Pieters, C.M., Keller, L.P., Morris, R.V., & McKay, D.S. (2001) Lunar mare soils: Space weathering and the major effects of surface correlated nanophase Fe. Journal of Geophysical Research, 106, 27,98527,999.CrossRefGoogle Scholar
Taylor, L.A., Pieters, C., Patchen, A., et al. (2010) Mineralogical and chemical characterization of lunar highland soils: Insights into the space weathering of soils on airless bodies. Journal of Geophysical Research, 115, E02002, DOI:10.1029/2009JE003427.CrossRefGoogle Scholar
Tompkins, S. & Pieters, C.M. (1999) Mineralogy of the lunar crust: Results from Clementine. Meteoritics and Planetary Science, 34, 2541.Google Scholar
Tompkins, S. & Pieters, C.M. (2010) Spectral characteristics of lunar impact melts and inferred mineralogy. Meteoritics and Planetary Science, 45, 11521169.Google Scholar
Van Gorp, B., Mouroulis, P., Blaney, D.L., Green, R.O., Ehlmann, B.L., & Rodriguez, J.I. (2014) Ultra-compact imaging spectrometer for remote, in situ, and microscopic planetary mineralogy. Journal of Applied Remote Sensing, 8, 084988.Google Scholar
Vane, G. (1993) Imaging spectrometry of the Earth and other Solar System bodies. In: Remote geochemical analysis: Elemental and mineralogical composition (Pieters, C.M. & Englert, P.A.J., eds.). Cambridge University Press, Cambridge, 121143.Google Scholar
Watson, K., Murray, B.C., & Brown, H. (1961) The behavior of volatiles on the lunar surface. Journal of Geophysical Research, 66, 30333045.Google Scholar
Yamamoto, S., Nakamura, R., Matsunaga, T., et al. (2010) Possible mantle origin of olivine around lunar impact basins detected by SELENE. Nature Geoscience, 3, 533–536.Google Scholar
Yamamoto, S., Matsunaga, T., Ogawa, Y., et al. (2011) Preflight and in-flight calibration of the spectral profiler on board SELENE (Kaguya). IEEE Transactions on Geoscience and Remote Sensing, 49, 4660–4676.Google Scholar
Yamamoto, S., Matsunaga, T., Ogawa, Y., et al. (2014) Calibration of NIR 2 of spectral profiler onboard Kaguya/SELENE. IEEE Transactions on Geoscience and Remote Sensing, 52, 68826898.Google Scholar
Yamamoto, S., Nakamura, R., Matsunaga, T., et al. (2015) Featureless spectra on the Moon as evidence of residual lunar primordial crust. Journal of Geophysical Research, 120, 21902205.Google Scholar

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×