Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (1): 70-86.doi: 10.13278/j.cnki.jjuese.20160258

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Sulfur and Lead Isotopic Composition and Their Ore-Forming Material Source of Skarn Copper Polymetallic Deposits in Southern Tibet Bangonghu-Nujiang Metallogenic Belt

Wu Denghao1,2, Gao Shunbao1, Zheng Youye1,3, Tian Kan3, Zhang Yongchao1, Jiang Junsheng3, Yu Zezhang3, Huang Pengcheng3   

  1. 1. Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China;
    2. Guizhou Mineral Geothermal Investment Co., Ltd, Guiyang 550007, China;
    3. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
  • Received:2017-05-24 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Key R&D Plan(2016YFC0600300) and Programme for Changjiang Scholars and Innovative Research Team in University (IRT14R54)

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Abstract: Numerous skarn Cu polymetallic deposits are discovered in the southern Bangonghu-Nujiang suture zone (BNSZ), which are related to the Bangonghu-Nujiang Middle Tethys Ocean southward subduction, collision, and post-collision. There are a lot of researches on a single deposit, but not on the contrast between two deposits. The authors systematically summarized the characteristics of S and Pb isotope of these deposits in combination with the previous researches on the Re isotope, the geochemical characteristics of metallogenic rock body, rock-forming and ore-forming age, and regional tectonic evolution, and took the contrasts between deposits into the study on the ore-forming materials of these deposits formed under different tectonic backgrounds. The results show that the δ34S values of Shesuo deposit present a notable bimodel distribution,which can be explained by the mixing of stratum and mantle. In summary, the 34S values were gradually enriched from the oceanic crust subduction stage (Shesuo), through the plate collision stage (Galale and Gaerqiong), to the post-collisional stage (Bangeria). The composition of Pb isotope indicates that the Shesuo deposit is enriched in radiogenic lead than the other deposits, and the ore forming material of Shesuo and Bangeria deposits were mainly sourced from the Nyainqentanglha group crystalline basement,while Galale and Gaerqiong deposits were from a mixture of crust-mantle materials, and the basement has a small contribution to the Gaerqiong deposit. In addition, the ore forming material of porphyry-skarn deposits has the characteristics of the mixture of crust-mantle materials, while the material of a skarn deposit mainly came from the upper crust.

Key words: S and Pb isotope, ore-forming materials sources, Bangonghu-Nujiang metallogenic belt, skarn copper polymetallic deposits, metallogenic environment

CLC Number: 

  • P618.4
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