Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (5): 1373-1386.doi: 10.13278/j.cnki.jjuese.20190276

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Genesis of M9 Ore Body of Basihu Pb-Zn Deposit in Qinghai Province: Constraints of Fluid Inclusions and H-O-S Isotopic Evidences

Sun Yonggang1,2, Li Bile1, Sun Fengyue1, Dong Junlin3, Qian Ye1, Yao Zhen3   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Geological Survey Institute of Jilin Province, Changchun 130102, China;
    3. No.5 Geologic Exploration and Mineral Resource Institute of Qinghai Province, Xining 810012, China
  • Received:2019-12-18 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by National Natural Science Foundation of China (41272093,41272095) and Project of China Geological Survey (12120114080901)

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Abstract: Basihu Pb-Zn deposit is located in Tuotuohe area of Qinghai Province in the northern part of Sanjiang polymetallic metallogenic belt. The M9 Pb-Zn ore body is hosted by the cataclastic alterated limestone and micrite of the Lower Permian Jiushidaoban Formation, and the main ore-controlling structure is the NWW trending fault that cuts through the formation. The mineralization process can be divided into three stages: Quartz-pyrite stage (Ⅰ), quartz-barite-polymetallic sulfide stage (Ⅱ), and carbonate-quartz stage (Ⅲ). The ore-forming fluid inclusions are dominated by gas-liquid two-phase fluid inclusions. The homogenization temperatures of fluid inclusions in stage I range from 315.1 to 365.9 ℃, with salinities (w (NaCl)) of 8.81%-11.46%. In stage Ⅱ, the homogenization temperatures range from 231.1 to 294.3 ℃, with salinities of 4.80%-10.49%. And in stage Ⅲ, the homogenization temperatures range from 155.1 to 233.7 ℃, with salinities of 2.41%-6.88%, indicating a typical medium temperature and low salinity fluid. The temperature and salinity decreased gradually from early to late mineralization. The H-O isotope data show that the mineralizing fluid was a mixture of magmatic water and meteoric water, mainly magmatic water in the early stage and mixed with meteoric water in the later stage. The S isotope data indicate that the ore-forming material source was related to the deep potassium magmatic activity in Cenozoic. The genetic type of M9 ore body in Basihu Pb-Zn deposit was a mesothermal hydrothermal vein type, and was formed in an extensional environment related to the late stage of the intracontinental orogenesis resulting from the India-Asia collision.

Key words: Tuotuohe area, fluid inclusions, H-O-S isotopes, hydrothermal vein deposit, Basihu Pb-Zn deposit

CLC Number: 

  • P618.4
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