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Stress-time context of fault permeability at the Krasnokamensk Area SE Transbaikalia
2013
Journal of Physics, Conference Series
The main aim of the contribution is to combine data on the consecutive stages of deformation, inflow and migration of palaeofluids and accumulation of mineral filling with uranium traces within the faulted-fractured environment at the Krasnokamensk Area, SE Transbaikalia, Russia. Object of examination is a framework of fault zones transecting the Proterozoic-Paleozoic granitic unit to the extent of northwestern part of uranium-bearing Streltsovskaya caldera of Mesozoic age. Considerations of
doi:10.1088/1742-6596/416/1/012018
fatcat:eyp7hjlpcjcpvkymvjqyfrv3ui