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““Learning about the degree of aqueous alteration of NEOs from ...

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CONCLUSIONS<br />

• Laboratory analyses <strong>of</strong> <strong>the</strong> reflectance <strong>of</strong> Antarctic CCs provide useful<br />

information for remote characterization <strong>of</strong> <strong>the</strong> presumably complex<br />

surface <strong>of</strong> Marco Polo-R and Osiris-Rex missions<br />

– IR spectra provide very significant features and absorption bands that have<br />

direct application:<br />

• The depth <strong>of</strong> <strong>the</strong> OH bands are directly related with <strong>the</strong> extent <strong>of</strong> <strong>aqueous</strong> <strong>alteration</strong>: how much<br />

water is bounded in phyllosilicates<br />

• The distinctive features allow to make reasonable distinction <strong>of</strong> <strong>the</strong> different surface<br />

mineralogy (if it is a complex breccia)<br />

• Consequently, IR spectroscopy <strong>of</strong> <strong>the</strong> target in a small scale is essential for sampling pristine<br />

carbonaceous materials (Marco Polo-R goal)<br />

– Carbon-rich asteroids are sources <strong>of</strong> all biogenic elements and have minerals<br />

that probably syn<strong>the</strong>sized complex organics (Martins, 2011):<br />

• Some features <strong>of</strong> <strong>the</strong> most abundant organics are also identifiable by using high-res IR spectra<br />

• We thank NASA Meteorite Working group and JSC curators for<br />

providing us with <strong>the</strong> samples to complete <strong>the</strong>se analyses.

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