Abstract
Granites are widespread in the Nanling region of China, which were emplaced in different tectonic environments as a result of frequent and intense magmatic activity. Two evolution sequences have been distinguished: the extrusive-hypabyssal and plutonic-hypabyssal sequences. Different mechanisms governing the evolution, especially the differentiation, of the two sequences may account for the different mechanisms of uranium mineralization leading to the formation of various types of uranium deposits in the Nanling region.
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