Age, geochemistry, mineralization, and tectonic significance of felsic-intermediate dikes in Shuangqishan Au deposit, Cathaysia block, South China

The Shuangqishan Au deposit (>15 t) is located in the Dehua-Youxi-Yongtai goldfield of the southeastern Cathaysia Block, South China. There are three stages of granites in the Shuangqishan Au deposit, the pre-mineralization granite porphyry formed in the Middle Jurassic (similar to 166.0 +/- 0.8 Ma), the metallogenic granite porphyry and monzonite porphyry formed in the late stage of the Late Jurassic (153-151 Ma), the post-mineralization granites (granite porphyry, the masanophyre, the dioritic porphyrite) formed in the Early Cretaceous (129.0-120.0 Ma). All rocks are characterized by high-K calc-alkaline and shoshonities series, the per-mineralization granites are enriched in Rb, Th, K, Zr, and Hf, depleted in Ba, P, and Ti, significant negative Eu anomaly and distinctly tetrad effect with highly fractionated I-type granitoids characteristics. The metallogenic granites and the post-mineralization granite porphyry are enriched in K, Rb, Th, Ce, Zr, Hf, and Y, enriched in LREE, strongly depleted in Sr, Ba Ta, P, Ti, have moderate negative Eu anomalies with I-type granites characteristics. However, the post-mineralization dioritic porphyrite displays strong depletions Sr, Ta, P, and Ti whereas Rb, Th, Ce, and Sm are enriched, enriched in LREE with weakly negative Eu anomalies. The metallogenic granite porphyry is significantly enriched in Au, As, Sb, W, Mo, and Bi, especially enriched in Au. The Lu-Hf isotopic data indicate that the magma source comes from the partial melting of the Paleoproterozoic crust, the minor part from the mantle in the Early Cretaceous. Therefore, we propose that the granitoids formed in the subducted plate environment from the Middle Jurassic to the Early Cretaceous, the Late Jurassic I-type granites (similar to 153-146 Ma), The Shuangqishan Au deposit was formed in the stage from compression to extension, the Early Cretaceous granites (similar to 129-114 Ma) mainly formed in the extensional environment and destroyed gold ore bodies.