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

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PRELIMINARY RESULTS<br />

• Significant differences in <strong>the</strong> reflectance spectra <strong>of</strong> CCs reflects a<br />

remarkable compositional diversity<br />

– The ATR technique is very sensitive to OH and o<strong>the</strong>r bonds absorption bands, but<br />

also provides information <strong>about</strong> organic features<br />

• CC groups exhibit components with distinctive abundance ratios<br />

– Chondrules are <strong>the</strong> abundant ingredients, but <strong>the</strong>y vary in average size and<br />

proportions, such as <strong>the</strong> Ca-Al rich inclusions (CAIs) and o<strong>the</strong>r components<br />

– Metal grain abundances are highly variable <strong>from</strong> being almost absent to ubiquitous<br />

depending <strong>of</strong> <strong>the</strong> chondrite group, and <strong>the</strong>ir presence inside <strong>the</strong> chondrules or in <strong>the</strong><br />

matrix has direct implications to reflectance<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> Marco Polo-R target<br />

– An accurate IR spectrum provides very significant features and<br />

absorption bands that have 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>:<br />

how much 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<br />

pristine carbonaceous materials (Marco Polo-R goal)

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