VARIATION OF THE MIDDLE INFRARED SPECTRAL REFLECTANCE CHARACTERISTICS OF CARBONATE ROCKS ON TECTONIC BELT;
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<正> Ⅰ. THE MIDDLE INFRARED SPECTRAL REFLECTANCE CHARACTERISTICS OF CARBONATE ROCKS The middle infrared reflective spectral response curves for the minerals of carbonate rocks are usually fairly distinct, and the spectral reflectance characteristic crests of the minerals from different areas are approximately the same. Fig. 1 is the middle