Characterization of Clay Minerals in the Athabasca Basin Using Shortwave Infrared (SWIR) Reflective Spectroscopy
This thesis presents results of a short-wave infrared (SWIR) reflectance spectroscopic study of clay minerals from the Athabasca Basin. Clay minerals (dickite, kaolinite, illite, and chlorite) are widespread in the Athabasca Basin and are particularly abundant in the alteration haloes associated wit...
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2015
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| Online Access: | http://hdl.handle.net/10388/6745 |