吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (5): 1354-1367.doi: 10.13278/j.cnki.jjuese.201605108

• 地质与资源 • 上一篇    下一篇

内蒙古额尔古纳地区八大关铜钼矿床流体包裹体特征与成矿时代

王晰1,2, 段明新3, 任云生1, 侯召硕4, 孙德有1, 郝宇杰1   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林大学应用技术学院, 长春 130022;
    3. 武警黄金第三支队, 哈尔滨 150069;
    4. 吉林省地质调查院, 长春 130061
  • 收稿日期:2015-10-20 出版日期:2016-09-26 发布日期:2016-09-26
  • 通讯作者: 任云生(1969-),男,教授,博士生导师,主要从事矿床学以及矿产普查与勘探的教学与研究工作,E-mail:renys@jlu.edu.cn E-mail:renys@jlu.edu.cn
  • 作者简介:王晰(1979-),男,讲师,博士研究生,主要从事矿床学的教学与研究工作,E-mail:xiwang@jlu.edu.cn
  • 基金资助:

    中国地质调查局项目（1212011121081）；中国核工业地质局项目（201151）

Characteristics of Fluid Inclusions and Mineralization Age of Badaguan Cu-Mo Deposit in Erguna Area, Inner Mongolia

Wang Xi1,2, Duan Mingxin3, Ren Yunsheng1, Hou Zhaoshuo4, Sun Deyou1, Hao Yujie1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Applied Technology College, Jilin University, Changchun 130022, China;
    3. No.3 Gold Geological Party of CAPF, Harbin 150069, China;
    4. Jilin Institute of Geology Survey, Changchun 130061, China
  • Received:2015-10-20 Online:2016-09-26 Published:2016-09-26
  • Supported by:

    Supported by the China Geological Survey Project (1212011121081);China's Nuclear Industry Geological Survey Project (201151)

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摘要：

八大关铜钼矿床为内蒙古额尔古纳地区发现较早但研究程度较低的典型斑岩型矿床。为确定其成矿机制、形成时代和构造背景，对主成矿阶段矿石脉石英中的流体包裹体开展了岩相学、显微测温、气相组分的激光拉曼光谱分析，利用LA-ICP-MS锆石U-Pb法和辉钼矿Re-Os法分别测定了成矿石英闪长斑岩体和铜钼矿石的同位素年龄。结果表明：八大关铜钼矿床成矿流体为中高温、中低盐度、中低密度的NaCl-H2O-CO2±CH4流体体系，流体的沸腾作用是矿床形成的重要机制；成矿石英闪长斑岩体的锆石U-Pb同位素年龄的加权平均值为（217.6±2.6）Ma，矿石中辉钼矿的Re-Os模式年龄为（222.4±3.3）Ma，因此八大关矿床的成岩成矿作用发生于晚三叠世。综合本文获得的成岩成矿年龄及前人在区域构造演化方面的研究资料认为，八大关矿床形成于与洋壳俯冲有关的活动大陆边缘构造背景，与蒙古-鄂霍茨克洋向南俯冲所引起的构造-岩浆活动具有密切的成因联系。

关键词: 流体包裹体, 同位素测年, 矿床成因, 构造背景, 八大关铜钼矿床, 内蒙古额尔古纳地区

Abstract:

The Badaguan porphyry copper-molybdenum deposit was discovered early, but has been low-degree researched. To determine its ore-forming fluid and mineralization mechanism, fluid inclusions in quartz grains from the ore are analyzed, including petrographic characteristics, microthermometry and gas compontents. LA-ICP-MS zircon U-Pb dating of metallogenic quartz diorite porphyry and Re-Os isotopic dating of molybdenite mineral have been carried out. The Badaguan deposit is charactered by the veinlet, network and veinlet-disseminated mineralization and facial zonation of wall-rock alterations, which are similar with those of the porphyry deposits. The ore-forming fluid is of medium- low-density, medium-low-salinity, medium-high-temperature NaCl-H2O-CO2±CH4 fluid system, fluid boiling might be an important mechanism for the formation of mineral deposits. Weighted mean U-Pb age of zircon grains from the metallogenic quartz diorite porphyry is (217.6±2.6)Ma, and Re-Os model age of the molybdenite is (222.4±3.3)Ma, which indicates that the metallogenic intrusion and associated copper-molybdenum mineralization took place in Late Triassic. Moreover, according to the geochemical characteristics and previous data in tectonic environment of the metallogenic porphyry in this area, authors propose that the Badaguan deposit may be resulted from tectonic-magmatism induced by southward subduction of the Mongolia-Okhotsk ocean. These conclusions are very significant for discussion of regional metallogenic regularities and metallogeny in board area among China, Russia and Mongolia.

Key words: fluid inclusion, isotopic dating, ore genesis, tectonic setting, Badaguan Cu-Mo deposit, Erguna area in Inner Mongolia

中图分类号: 

  • P618.41

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