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Extra resources for Spectroscopy of Rocks and Minerals, and Principles of Spectroscopy

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Combination and overtone bands of the CO3 fundamentals occur in the near IR. g. Figure 10a). g. g. Hunt and Salisbury, 1971). , 1993). An example of such a band shift is seen in Figures 10a, 11 and, in more detail, Figure 24a showing the shift in absorption position from calcite to dolomite. 3 Other Minerals. Phosphates, borates, arsenates, and vanadates also have diagnostic vibrational spectra. Space precludes inclusion of spectra here. , (1993b) for visual to near-infrared spectra. g. P-O stretch) occurs at mid-infrared wavelengths.

2-µm band. 2-µm features for halloysite and kaolinite are shown in Figure 24b, where we can see significant differences between the spectra of the two minerals. Figure 24a. Figure 24a: 20k 100dpi gif Figure 24a: 65k 200dpi gif Figure 24a: 128k 300dpi gif Figure 24a. Comparison of calcite and dolomite continuum-removed features. The dolomite absorption occurs at a shorter wavelength than the calcite absorption. refl-mrs/ (58 of 77) [9/19/2002 10:11:29 PM] USGS Spectroscopy Lab: Spectroscopy of Rocks and Minerals, and Principles of Spectroscopy Figure 24b.

G. Figure 10a). g. g. Hunt and Salisbury, 1971). , 1993). An example of such a band shift is seen in Figures 10a, 11 and, in more detail, Figure 24a showing the shift in absorption position from calcite to dolomite. 3 Other Minerals. Phosphates, borates, arsenates, and vanadates also have diagnostic vibrational spectra. Space precludes inclusion of spectra here. , (1993b) for visual to near-infrared spectra. g. P-O stretch) occurs at mid-infrared wavelengths. However, many of these minerals contain OH or H20 and have absorptions in the near-infrared.

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