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Fig. 10

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Genetic model of the Muping–Rushan gold belt (modified from (Deng et al., 2020a; Deng et al., 2020b; Lei et al., 2018)). (a) Late Jurassic (160∼140 Ma) magmatic activity, Kunyushan granitic complex emplacement; (b) Early Cretaceous (120∼110 Ma) magmatic activity, emplacement of the Sanfoshan granite and arc-related mafic dyke; (c) Subsequently (110∼100 Ma), the gold mineralization process of Muping–Rushan gold belt.

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