Abstract
The fission track (f.t.) age determinations of garnet occuring in copper ore deposits of Khetri copper belt, Rajasthan and Singhbbum copper belt, Bihar reveal the metamorphism of copper ore formations of these areas. The f.t. age of garnet from Khetri copper belt varies from 831 to 897 m.y. suggesting the occurence of last metamorphism in the belt corresponding to Delhi system. The f.t. age of garnet from Bihar copper belt is found to be 1014 m.y. which corresponds to the Satpura cycle. The maximum enrichment of uranium is observed in copper ore formations of Bihar.
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Schedule a callMore From: International Journal of Radiation Applications and Instrumentation. Part D. Nuclear Tracks and Radiation Measurements
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