In-situ elemental and isotopic compositions of apatite and zircon from the Shuikoushan and Xihuashan granitic plutons: Implication for Jurassic granitoid-related Cu-Pb-Zn and W mineralization in the Nanling Range, South China

• Published in: Ore geology reviews Vol. 93; pp. 382 - 403
• Main Authors: Yang, Jie-Hua, Kang, Li-Fang, Peng, Jian-Tang, Zhong, Hong, Gao, Jian-Feng, Liu, Liang
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.02.2018
• Subjects: Apatite and zircon; Cu-Pb-Zn and W mineralization; In-situ elemental and isotopic compositions; Nanling Range; South China; Xihuashan and Shuikoushan plutons; Xihuashan and Shuikoushan plutons; Cu-Pb-Zn and W mineralization; Nanling Range; Apatite and zircon; In-situ elemental and isotopic compositions; South China
• ISSN: 0169-1368; 1872-7360
• DOI: 10.1016/j.oregeorev.2017.12.023

[Display omitted] •Shuikoushan and Xihuashan plutons intruded at 158.8 Ma and 155.6 Ma, respectively.•The two plutons likely generated from different crustal level.•Oxidized and reduced magmas related to Cu-Pb-Zn and W deposits, respectively.•Magmatic origin and evolution controlled diverse granitoid-related mineralization. The Nanling Range, South China, was world-famous for hosting abundant granitoid-related copper-lead-zinc (Cu-Pb-Zn) polymetallic ore deposits and quartz vein-type wolframite (W) ore deposits, both of which have roughly similar formation ages predominately between 150 and 160 Ma with a peak of ca. 156 Ma. In this study, accessory minerals from typical Cu-Pb-Zn-bearing and W-bearing granitic rocks are compared in terms of elemental and isotopic compositions. Apatite from W-bearing granites in the Xihuashan pluton has lower εNd(t) value (−11.9 to −8.6) than that from Cu-Pb-Zn-bearing granitic rocks in Shuikoushan with εNd(t) value of −8.7 to −4.2 and initial 87Sr/86Sr ratio of 0.7097–0.7109. Zircon grains in Xihuashan, yielded εHf(t) value from −14.9 to −11.4, δ18O value from 8.6‰ to 10.4‰, and highly variable and negative δ7Li value (−45.8‰ to −3.8‰), whereas those in Shuikoushan have relatively higher εHf(t) value (−10.6 to −8.1), lower δ18O value (8.4‰–9.7‰), and highly variable δ7Li values from −12.7‰ to +17.6‰. In situ Hf-O-Li isotopic compositions of zircon and Sr-Nd isotopes of apatite, suggesting that the Shuikoushan granitic pluton was likely generated from dehydration melting of amphibolite from a metal-fertile mafic source in the middle-to-lower crust, whereas the Xihuashan granitic pluton could be derived from partial melting of metapelite with minor amphibolite in the middle to upper crust. The geochemical records in accessory minerals fingerprint that the Shuikoushan granitic magma was characterized by high Cl content (0.11–1.44 wt%) and logfo2 value (>ΔFMQ+1), whereas the Xihuashan granitic magma have elevated F (3.51–4.80 wt%) and Li (3.49–42.4 ppm) contents with low logfo2 value (<FMQ+0), which suggested moderately oxidized magmas with high Cl contents are in favor of the formation of magmatic-hydrothermal Cu-Pb-Zn deposits, whereas weakly reduced magmas with high F and Li contents could be involved in the formation of the quartz vein-type wolframite deposits. In conclusion, different source rocks and magmatic evolution processes are the key to the understanding of the Jurassic diverse granitoid-related mineralization in the Nanling Range.