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Asteroid Spectroscopy

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Clay Mineral Spectra<br />

S. J. Gaffey et al. (1993)<br />

The narrow absorption features<br />

near 1.4, 1.9, 2.2-2.3, 2.5 µm (etc.)<br />

are produced by vibrational<br />

overtones of the H 2 O and OH<br />

molecules.<br />

Their shape and exact position<br />

depends on the crystal structure<br />

and the attached cations.<br />

These spectra parameters are<br />

diagnostic of specific minerals.

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