Two periods of mineralization in Xiaoxinancha Au-Cu deposit, NE China: evidences from the geology and geochronology

• Published in: Geological journal (Chichester, England) Vol. 51; no. 1; pp. 51 - 64
• Main Authors: Zeng, Qingdong, Guo, Feng, Zhou, Lingli, Duan, Xiaoxia
• Format: Journal Article
• Language: English
• Published: Liverpool Blackwell Publishing Ltd 01-01-2016; Wiley Subscription Services, Inc
• Subjects: NE China; porphyry Au-Cu mineralization; Re-Os age; SHRIMP U-Pb age; Xiaoxinancha deposit; China, People's Rep
• ISSN: 0072-1050; 1099-1034
• DOI: 10.1002/gj.2605

The Xiaoxinancha Au–Cu deposit is located at the eastern segment of the Tianshan–Xingmeng orogenic belt in northeast China. The deposit includes porphyry Au–Cu orebodies, veined Au–Cu orebodies and veined Mo mineralizations. All of them occur within the diorite intrusion. The Late Permian diorite, Late Triassic granodiorite, Early Cretaceous granite and granite porphyry are developed in the ore area. The studies on geological features show that the porphyry Au–Cu mineralization is related to the Late Permian diorite intrusion. New geochronologic data for the Xiaoxinancha porphyry Au–Cu deposit yield Permian crystallization zircon U–Pb age of 257 ± 3 Ma for the diorite that hosts the Au–Cu mineralization. Six molybdenite samples from quartz + molybdenite veins imposed on the porphyry Au–Cu orebodies yield an isochron age of 110.3 ± 1.5 Ma. The ages of the molybdenites coeval to zircon ages of the granite within the errors suggest that the Mo mineralization was genetically related to the Early Cretaceous granite intrusion. The formation of the diorite and the related Au–Cu mineralization were caused by the partial melting of the subduction slab during the Late Palaeozoic palaeo‐Asia Ocean tectonic stage. The Re contents and Re–Os isotopic data indicate that the crustal resource is dominated for the Mo mineralization during the Cretaceous extensional setting caused by the roll‐back of the palaeo‐Pacific plate. Copyright © 2014 John Wiley & Sons, Ltd.