Evolutionary characteristics of the U-Pb isotopic system in a certain uranium deposit in North Guangdong—A discussion on the model for its genesis

Based on the evolutionary theory of U-Pb isotopic system, we have studied the genetic model for a uranium deposit occurring in carbonate-silicolite-pelite. The data show that the U-deposit is characterized by a multi-stage evolution with respect to its U-Pb isotopic system, and the mechanism of its genesis can be explained by later repeated superimposition of mine-ralization which took place at about 200±10m. y., 100±10m. y., 60±10m. y. and 11±1m. y. ago. These mineralization stages are closely related to regional tectonic activities.