Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (4): 1050-1070.doi: 10.13278/j.cnki.jjuese.20170092

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Genesis of Zhuxi Copper-Tungsten Deposit in Jiangxi Province: Insights from Mineralogy and Chronology

He Xiaolong1, Zhang Da1, Chen Guohua2, Di Yongjun1, Huo Hailong1,3, Li Ning1, Zhang Zhihui1,4, Rao Jianfeng2, Wei Jin2, Ouyang Yongpeng2   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. 912 Geological Team, Bureau of Geology and Mineral Resources of Jiangxi Province, Yingtan 335001, Jiangxi, China;
    3. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;
    4. Research and Development Center, China Geological Survey, Beijing 100120, China
  • Received:2017-09-25 Online:2018-07-26 Published:2018-07-26
  • Supported by:
    Supported by Public Welfare Foundation for Scientific Researchin the Ministry of Land and Resources(201411035-3)

Abstract: The Zhuxi deposit is located in Jingdezhen in Jiangxi Province, which is a world-class super large copper-tungsten deposit,and its genesis remain debated. The research on the geological characteristics, skarn mineralogy and ore-bearing rock chronology show that the orebodies occur in the unconformity interface between the marble of the Upper Carboniferous Huanglong Group and the metamorphic rocks of the Neoproterozoic Shuangqiaoshan Group, and have significant mineral assemblage zonage with the surrounding rocks. According to the skarn occurrence, mineral association, metasomatic and petrographic characteristics, from early to late the mineralization was divided into skarn stage, retrograde alteration stage, quartz-sulfide stage, and carbonate stage. The representative skarn minerals are garnet, diopside, tremolite, wollastonite, vesuvianite, serpentine, chlorite, etc. The electron microprobe analysis shows that the garnet belongs to grossularite-andradite series, and the pyroxene mainly belongs to diopside-andradite series. The study of isotopic chronology and the relationship between magma and mineralization show that the granodiorite is related to the early skarn-type mineralization, and its scale is smaller and the ore grade is low;the biotite granite is related to the greisen-type and late skarn type mineralization with a wide scale and high ore grade. The result of LA-ICP-MS zircon U-Pb dating of the biotite granite is (147.7±2.2)Ma. The comprehensive analysis shows that the Zhuxi copper-tungsten deposit is formed by the multi-stage metasomatism of the Late Jurassic granitic magma related hydrothermal and Late Paleozoic carbonate rocks, and the mineralization is characterized by skarn-type and greisen-type mainly.

Key words: Zhuxi copper-tungsten deposit, mineralogy, metallogenic mode, electron microprobe, zircon U-Pb dating

CLC Number: 

  • P618
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