Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (5): 1354-1367.doi: 10.13278/j.cnki.jjuese.201605108

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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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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

CLC Number: 

  • P618.41

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