69 Mars Rover Curiosity: Geoscience in Gale Crater
Monday, 5 November 2012
8:00 AM - 12:00 PM
Ballroom B
THE CHEMCAM INVESTIGATION: COMPOSITIONS AT THE CURIOSITY ROVER LANDING SITE
Paper number: 69-12
Program: Technical Sessions
Time: 11:05 AM – 11:20 AM
Authors
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Sylvestre MauriceInstitut de Recherche en Astrophysique et Planetologie, Toulouse
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MSL Science TeamJet Propulsion Laboratory, Pasadena, CA
Abstract
ChemCam’s LIBS analyses are semi-quantitative, as abundance determinations rely on comparison with training-set spectra and cross calibration with APXS. Key features of the technique as applied to field geology on Mars are the ability to remove surface dust with repeated laser pulses at the same location and to probe samples for surface coatings or weathering rinds. Depth profiling proceeds at a rate of approximately one micron per pulse for many rocks, and ChemCam can profile up to a few cm into unconsolidated soils. Line scans and rasters can be used to determine sample heterogeneity or to walk up a sequence of layers.
Gale Crater was selected as the Curiosity landing site based on the 5 km of sedimentary strata that comprises Mt. Sharp at the center of the crater and based on the evidence for flowing and potentially standing water within and near the landing ellipse. The actual landing site is within 400 m of a junction of several different geological terrains having differing thermal inertias and elevations, suggesting the potential for interesting targets for study early in the mission.