Spectral and mineralogical effects of heating on CM chondrite and related asteroids
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T. Hiroi | E. Cloutis | V. Reddy | S. Mertzman | D. Applin | K. Mengel | T. Kareta | P. Beck | P. Mann | S. Sidhu
[1] A. Davis,et al. Samples returned from the asteroid Ryugu are similar to Ivuna-type carbonaceous meteorites , 2022, Science.
[2] M. Mermoux,et al. Geologically rapid aqueous mineral alteration at subfreezing temperatures in icy worlds , 2022, Nature Astronomy.
[3] C. Pilorget,et al. First compositional analysis of Ryugu samples by the MicrOmega hyperspectral microscope , 2021, Nature Astronomy.
[4] C. Pilorget,et al. Preliminary analysis of the Hayabusa2 samples returned from C-type asteroid Ryugu , 2021, Nature Astronomy.
[5] V. Reddy,et al. Investigating the Relationship between (3200) Phaethon and (155140) 2005 UD through Telescopic and Laboratory Studies , 2021, The Planetary Science Journal.
[6] D. Reuter,et al. Weak spectral features on (101995) Bennu from the OSIRIS-REx Visible and InfraRed Spectrometer , 2020, Astronomy & Astrophysics.
[7] E. Cloutis,et al. Phase reddening on asteroid Bennu from visible and near-infrared spectroscopy , 2020, Astronomy & Astrophysics.
[8] D. DellaGiustina,et al. In situ evidence of thermally induced rock breakdown widespread on Bennu’s surface , 2020, Nature Communications.
[9] Makoto Yoshikawa,et al. Hayabusa2 mission status: Landing, roving and cratering on asteroid Ryugu , 2020, Acta Astronautica.
[10] M. Granvik,et al. New Evidence for a Physical Link between Asteroids (155140) 2005 UD and (3200) Phaethon , 2020, The Planetary Science Journal.
[11] B. Schmitt,et al. Style and intensity of hydration among C-complex asteroids: A comparison to desiccated carbonaceous chondrites , 2020, 2004.09872.
[12] S. Kamali,et al. Quantitative determination of magnetite and maghemite in iron oxide nanoparticles using Mössbauer spectroscopy , 2019, SN Applied Sciences.
[13] H. Busemann,et al. The Yamato-type (CY) carbonaceous chondrite group: Analogues for the surface of asteroid Ryugu? , 2019, Geochemistry.
[14] M. Yamada,et al. The surface composition of asteroid 162173 Ryugu from Hayabusa2 near-infrared spectroscopy , 2019, Science.
[15] R. Jaumann,et al. Hayabusa2 arrives at the carbonaceous asteroid 162173 Ryugu—A spinning top–shaped rubble pile , 2019, Science.
[16] W. Bottke,et al. DISRUPTION AND REACCUMULATION AS THE POSSIBLE ORIGIN OF RYUGU AND BENNU TOP SHAPES , 2019 .
[17] M. K. Crombie,et al. Evidence for widespread hydrated minerals on asteroid (101955) Bennu , 2019, Nature Astronomy.
[18] M. K. Crombie,et al. The Unexpected Surface of Asteroid (101955) Bennu , 2019, Nature.
[19] A. Verchovsky,et al. The alteration history of the Jbilet Winselwan CM carbonaceous chondrite: An analog for C‐type asteroid sample return , 2018, Meteoritics & Planetary Science.
[20] J. Zipfel,et al. Composition, petrology, and chondrule‐matrix complementarity of the recently discovered Jbilet Winselwan CM2 chondrite , 2018, Meteoritics & Planetary Science.
[21] E. Cloutis,et al. Ultraviolet spectral reflectance of carbonaceous materials , 2018, Icarus.
[22] S. Steinbach,et al. Fe isotope composition of bulk chondrules from Murchison (CM2): Constraints for parent body alteration, nebula processes and chondrule-matrix complementarity , 2018 .
[23] M. K. Crombie,et al. OSIRIS-REx: Sample Return from Asteroid (101955) Bennu , 2017, Space Science Reviews.
[24] S. Berensmeier,et al. Oxidation of magnetite nanoparticles: impact on surface and crystal properties , 2017 .
[25] Everett Shock,et al. Carbonaceous Chondrite Meteorites: the Chronicle of a Potential Evolutionary Path between Stars and Life , 2017, Origins of Life and Evolution of Biospheres.
[26] Richard P. Binzel,et al. The geophysical environment of Bennu , 2016 .
[27] Jonathan Gal-Edd,et al. The OSIRIS-REx asteroid sample return mission , 2015, 2015 IEEE Aerospace Conference.
[28] D. Vokrouhlický,et al. Orbit and bulk density of the OSIRIS-REx target Asteroid (101955) Bennu , 2014, 1402.5573.
[29] M. Zolensky,et al. Petrographic, chemical and spectroscopic evidence for thermal metamorphism in carbonaceous chondrites I: CI and CM chondrites , 2014 .
[30] Y. Tsuda,et al. System design of the Hayabusa 2—Asteroid sample return mission to 1999 JU3 , 2013 .
[31] Harry Y. McSween,et al. Nature and degree of aqueous alteration in CM and CI carbonaceous chondrites , 2013 .
[32] O. Mosin,et al. The structure and composition of natural carbonaceous fullerene containing mineral shungite , 2013 .
[33] Paul Mann,et al. Spectral reflectance properties of carbonaceous chondrites: 1. CI chondrites , 2012 .
[34] M. Gaffey,et al. Spectral reflectance properties of carbonaceous chondrites 4: Aqueously altered and thermally metamorphosed meteorites , 2012 .
[35] A. Gualtieri,et al. The dehydroxylation of serpentine group minerals , 2012 .
[36] P. Bland,et al. Modal mineralogy of CM chondrites by X-ray diffraction (PSD-XRD): Part 2. Degree, nature and settings of aqueous alteration , 2011 .
[37] P. Michel,et al. TEMPERATURE HISTORY AND DYNAMICAL EVOLUTION OF (101955) 1999 RQ 36: A POTENTIAL TARGET FOR SAMPLE RETURN FROM A PRIMITIVE ASTEROID , 2011 .
[38] M. Vázquez,et al. Magnetic Iron Oxide Nanoparticles in 10−40 nm Range: Composition in Terms of Magnetite/Maghemite Ratio and Effect on the Magnetic Properties , 2011 .
[39] P. Michel,et al. Orbital and thermal evolutions of four potential targets for a sample return space mission to a primitive near-Earth asteroid , 2010 .
[40] G. Cody,et al. Deuterium enrichments in chondritic macromolecular material—Implications for the origin and evolution of organics, water and asteroids , 2010 .
[41] B. Schmitt,et al. Hydrous mineralogy of CM and CI chondrites from infrared spectroscopy and their relationship with low albedo asteroids , 2010 .
[42] R. Okazaki,et al. Thermal Metamorphism of CM Carbonaceous Chondrites: Effects on Phyllosilicate Mineralogy and Presolar Grain Abundances , 2006 .
[43] Tomoki Nakamura. Post-hydration thermal metamorphism of carbonaceous chondrites , 2005 .
[44] A. Rubin. What heated the asteroids? , 2005, Scientific American.
[45] M. Sephton,et al. Organic compounds in carbonaceous meteorites. , 2002, Natural product reports.
[46] M. Zolensky,et al. Petrographic, Chemical and Spectroscopic Data on Thermally Metamorphosed Carbonaceous Chondrites , 2002 .
[47] H. McSween,et al. Thermal Evolution Models of Asteroids , 2002 .
[48] Bruce Hapke,et al. Space weathering from Mercury to the asteroid belt , 2001 .
[49] M. Zolensky,et al. UV-Vis-NIR absorption features of heated phyllosilicates as remote-sensing clues of thermal histories of primitive asteroids , 1999 .
[50] W. Bourcier,et al. Constraints on the anhydrous precursor mineralogy of fine‐grained materials in CM carbonaceous chondrites , 1998 .
[51] M. Zolensky,et al. Thermal metamorphism of the C, G, B, and F asteroids seen from the 0.7 μm, 3 μm, and UV absorption strengths in comparison with carbonaceous chondrites , 1996 .
[52] A. Rubin. Petrologic evidence for collisional heating of chondritic asteroids , 1995 .
[53] M. Zolensky,et al. Infrared diffuse reflectance spectra of carbonaceous chondrites: Amount of hydrous minerals , 1994 .
[54] M. Zolensky,et al. Possible thermal metamorphism on the C, G, B, and F asteroids detected from their reflectance spectra in comparison with carbonaceous chondrites , 1994 .
[55] M. Zolensky,et al. Evidence of Thermal Metamorphism on the C, G, B, and F Asteroids , 1993, Science.
[56] J. Breton,et al. The vis/UV spectrum of coals and the interstellar extinction curve , 1993 .
[57] F. Fanale,et al. Simulation of possible regolith optical alteration effects on carbonaceous chondrite meteorites , 1993 .
[58] Akai Junji. Mineralogical evidence of heating events in Antarctic carbonaceous chondrites, Y-86720 and Y-82162 , 1990 .
[59] R. Morris,et al. Spectral and other physicochemical properties of submicron powders of hematite (alpha-Fe2O3), maghemite (gamma-Fe2O3), magnetite (Fe3O4), goethite (alpha-FeOOH), and lepidocrocite (gamma-FeOOH). , 1985, Journal of geophysical research.
[60] H. McSween. Are carbonaceous chondrites primitive or processed? A review , 1979 .
[61] M. Lipschutz,et al. Thermal metamorphism of primitive meteorites. VI - Eleven trace elements in Murchison C2 chondrite heated at 400-1000 C , 1977 .
[62] John B. Adams,et al. Visible and near‐infrared diffuse reflectance spectra of pyroxenes as applied to remote sensing of solid objects in the solar system , 1974 .
[63] Torrence V. Johnson,et al. Optical properties of carbonaceous chondrites and their relationship to asteroids , 1973 .
[64] L. Fuchs,et al. Mineralogy, mineral-chemistry, and composition of the Murchison (C2) meteorite , 1973 .
[65] W. D. Ehmann,et al. CHEMICAL ANALYSES OF THE MURCHISON AND LOST CITY METEORITES , 1970 .