吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1373-1386.doi: 10.13278/j.cnki.jjuese.20190276

• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇    下一篇

青海省巴斯湖铅锌矿床M9矿体成因探讨——流体包裹体和H-O-S同位素约束

孙永刚1,2, 李碧乐1, 孙丰月1, 董峻麟3, 钱烨1, 姚振3   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林省地质调查院, 长春 130102;
    3. 青海省第五地质矿产勘查院, 西宁 810012
  • 收稿日期:2019-12-18 出版日期:2020-09-26 发布日期:2020-09-29
  • 作者简介:孙永刚(1988-),男,博士研究生,主要从事热液矿床成矿理论与预测研究,E-mail:xg429805791@163.com
  • 基金资助:
    国家自然科学基金项目（41272093，41272095）；中国地质调查局项目（12120114080901）

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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摘要： 巴斯湖铅锌矿床位于三江多金属成矿带北段的青海省沱沱河地区，M9铅锌矿体赋存于下二叠统九十道班组碎裂蚀变灰岩和泥晶灰岩中，主控矿构造为切割地层的NWW向断裂构造。成矿过程分为石英-黄铁矿阶段（Ⅰ）、石英-重晶石-多金属硫化物阶段（Ⅱ）和碳酸盐-石英阶段（Ⅲ）3个阶段。成矿流体包裹体以气液两相为主，成矿Ⅰ阶段均一温度为315.1~365.9℃，盐度（w（NaCl））为8.81%~11.46%；成矿Ⅱ阶段均一温度为231.1~294.3℃，盐度为4.80%~10.49%；成矿Ⅲ阶段均一温度为155.1~233.7℃，盐度为2.41%~6.88%。成矿流体为典型的中温、低盐度流体，均一温度和盐度从成矿早期到晚期逐渐降低。H-O同位素数据显示成矿流体为岩浆水和大气水的混合水，早期主要为岩浆水，晚期有大气降水的混入；S同位素数据显示成矿物质来源与新生代深部钾质岩浆活动有关。巴斯湖铅锌矿床M9矿体成因类型为中温热液脉型，形成于印度-欧亚板块晚碰撞造山作用引起的伸展环境。

关键词: 沱沱河地区, 流体包裹体, H-O-S同位素, 热液脉型矿床, 巴斯湖铅锌矿床

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

中图分类号: 

  • P618.4
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