T110 The Geology of Dwarf Planet Ceres
Monday, 26 September 2016
8:00 AM - 12:00 PM
Room 201
SURFICIAL COMPOSITION OF DWARF PLANET CERES
Paper number: T110-4
Program: Technical Sessions
Time: 8:35 AM – 8:55 AM
Authors
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Andrea RaponiIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Michael ToplisCentre National de la Recherche Scientifique, Toulouse
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Federico TosiIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Julie C. Castillo-RogezJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA
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Fabrizio CapaccioniIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Maria Teresa CapriaIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Sergio FonteIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Marco GiardinoIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Ralf JaumannInstitute of Planetary ResearchGerman Aerospace Center (DLR), Berlin
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Andrea LongobardoINAF - Istituto Nazionale di Astrofisica, Rome
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Maria Cristina De SanctisIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Thomas B. McCordBear Fight Institute, Winthrop, WA
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Lucy McFaddenNASA Goddard Space Flight Center, Greenbelt, MD
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Ernesto PalombaIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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C.M. PietersBrown University, Providence, RI
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Carol A. RaymondJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA
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Paul Schenkhouston, TX
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Francesca ZambonIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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C.T. RussellUniversity of California, Los Angeles, Los Angeles, CA
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Mauro CiarnielloIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Alessandro FrigeriIAPS - Istituto di Astrofisica e Planetologia Spaziali, Rome
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Filippo Giacomo CarrozzoINAF - Istituto Nazionale di Astrofisica, Rome
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Jean-Philippe CombeBear Fight Institute, Winthrop, WA
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Bethany EhlmannCalifornia Institute of Technology, MC170-25, Pasadena, CA
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Simone MarchiSouthwest Research Institute, Boulder, CO
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H.Y. McSweenUniversity of Tennessee, Knoxville, AZ
Abstract
The average thermally corrected reflectance spectrum of Ceres as measured by VIR shows that the spectrum in the 2.6–4.2μm region is compatible with the presence on the surface of a mixture of dark carbon-rich minerals, Mg- phyllosilicates, ammoniated clays, and carbonates [4]. This result confirms previous studies based on ground based spectra [5, 6].
The pervasive presence of Mg- and NH4-bearing phyllosilicates indicates endogenous formation by a globally widespread and extensive alteration processes while the variations in the amount of phyllosilicate suggest the existence of a vertically stratified upper crust [7].
The heterogeneity of the crust is also suggested by the presence of the ‘bright spots’. The typically dark surface of the dwarf planet Ceres is punctuated by areas of much higher albedo [8,9]. These areas are mostly consistent with a large amount of carbonate, implying recent hydrothermal activity [10].
References
[1] Russell C.T. and Raymond C.A. (2011) Space Sci. Rev., 163, 3–23. [2] Russell C.T. et al. (2016) Science. [3] De Sanctis M.C. et al. (2011) Space Sci. Rev., 163, 329–369. [4] De Sanctis M.C. et al. (2015) Nature. [5] King T. et al. (1992) Science, 255, 1551–1553. [6] Rivkin A.S. et al. (2006) Icarus, 185, 563–567. [7] Ammannito E. et al. (2016), Science. [8] Li, J.Y. et al. (2016) The Astrophysical Journal Letters, 817, 2, L22. [9] Ciarniello M. et al. (2016) MNRAS submitted. [10] De Sanctis et al. (2016), Nature.
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-285709
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