T239 Dawn at Vesta: Initial Results from the Survey Orbit
Wednesday, 12 October 2011
8:00 AM - 12:00 PM
Room L100H-J
4 VESTA MINERALOGY: SUGGESTIONS FROM VIR OBSERVATIONS
Paper number: T239-5
Program: Technical Sessions
Time: 9:15 AM – 9:30 AM
Authors
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Maria Cristina De SanctisIASF, Istituto di Astrofisica Spaziale e Fisica Cosmica, Rome, N/A
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Angioletta CoradiniIFSI, Istituto di Fisica dello Spazio Interplanetario, Rome, N/A
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Eleonora AmmannitoIFSI, Istituto di Fisica dello Spazio Interplanetario, Rome, N/A
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Fabrizio CapaccioniIASF, Istituto di Astrofisica Spaziale e Fisica Cosmica, Rome, N/A
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Maria Teresa CapriaIASF, Istituto di Astrofisica Spaziale e Fisica Cosmica, Rome, N/A
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Gianrico FilacchioneIASF, Istituto di Astrofisica Spaziale e Fisica Cosmica, Rome, N/A
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Thomas B. McCordBear Fight Institute, Winthrop, WA
Abstract
One of the main goals of Dawn is to determine the mineral composition of the surface and to place it in a geologic context. Several diagnostic absorption bands of key minerals occur in the visible and near-infrared regions. VIS and Near-IR spectroscopy contribute to asteroid studies by delineating absorption features that are not resolved with broad-band filters and by refining the evaluation of differences in terms of spectral shape and band depth and width. Maps of the current surface mineralogy will ultimately lead to the understanding of the surface evolution and determination of the processes affecting it.
Our present understanding of Vesta is based on telescopic remote sensing and the analysis of the HED meteorites, which are thought to be representative of Vesta as a whole. VIR data of materials exposed on the asteroid’s surface provide new insights into the processes that produced the solar system’s largest differentiated asteroid.