Abstract
From the fission track age deteimination of garnet occurring in copper ore deposits of Khetri copper belt, Rajasthan, it has been possible to reveal the metamorphism of copper ore formations of the area. The fission track age of 831 ± 132m.y. for garnet suggests that the copper ore formations in the region were subjected to a metamorphic episode which coincides with the Delhi Cycle. © 1980, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved.
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CITATION STYLE
Singh, S., & Virk, H. S. (1980). Fission track dating of copper ore formations of Khetri area, Rajasthan State (India). GEOCHEMICAL JOURNAL, 14(1), 51–55. https://doi.org/10.2343/geochemj.14.51
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