Neoproterozoic uranium-mineralized sedimentary rocks from the Kaladgi Basin, Dharwar Craton, southwestern India: source and transport mechanism of uranium
The Kaladgi Basin of the Dharwar Craton, southeast India, hosts Proterozoic unconformity-related uranium (U) mineralization controlled by faulted contacts between Archean basement and Proterozoic cover sediments. To understand the ore-forming processes, 25 core samples from the Cave Temple Arenite were analyzed using w...