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Intensely deformed and mylonitised rocks of the Almora Crystalline Zone (ACZ) have shown the potential of 238U and 232Th enrichment. 232Th, 238U and 40K are investigated by gamma-ray spectrometry in the rock samples collected along the three selected traverses across the North Almora Thrust Zone (NATZ). Obtained average values of U and Th are much higher, 7.3 and 23.9 ppm, respectively, than the average...
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