Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (4): 1071-1084.doi: 10.13278/j.cnki.jjuese.20170169

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Characteristics of Ore-Forming Fluid and Genesis of Baoxinggou Gold Deposit in North of Great Xing'an Range

Li Xiangwen1, Zhang Zhiguo2, Wang Keyong3, Sun Jiapeng3, Yang Jibo1, Yang He3   

  1. 1. No.3 Gold Geological Party of CAPF, Harbin 150086, China;
    2. Category Institute of CAPF, Beijing 102202, China;
    3. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2017-10-25 Online:2018-07-26 Published:2018-07-26
  • Supported by:
    Supported by Project of China Geological Survey (12120115041801) and Gold Job of Golden Commend of the Armed Police(2008-20140301)

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Abstract: The Baoxinggou gold deposit is a large-scale deposit in the upper Heilongjiang metallogenic belt in the north of Great Xing'an Range. The ore bodies mainly occur in the contact zone between the sandstone of the Early Jurassic Ershierzhan Formation and the Early Cretaceous quartz diorite, diorite porphyrite. The hydrothermal mineralization can be classified into three stages:pyrite±arsenopyrite-quartz (Ⅰ), polysulfide-quartz (Ⅱ) and sulfide-poor carbonate (Ⅲ). The petrographic study of the fluid inclusions showed that there were aqueous two phases (LV type), fewer CO2-bearing three phases (HCO2 type),and vapor-rich phases (FV type) fluid inclusions developed in the stage I; aqueous two phases (LV type) and fewer CO2-bearing three phases (HCO2 type) in the stage Ⅱ; only aqueous two phases (LV type) in the stage Ⅲ. The micro-thermometric research revealed that the peak homogeneous temperature of fluid inclusions in the stageⅠandⅡ was range of 225.00-300.00℃, the salinity was range of 2.00%-10.00% NaCl, and those in the stage Ⅲ were 175.00-225.00℃ and 4.00%-8.00% NaCl correspondingly. The ore-forming fluids were of CO2-bearing medium-low temperature and low salinity NaCl-H2O-CO2 system solutions; and with the progressing of mineralization, the temperature and salinity gradually decreased. The hydrogen and oxygen isotope analysis showed that the δDSMOW of mineralization stageⅠand stageⅡvaried in the range of -131.00‰-108.00‰, δ18OSMOW varied in the range of 1.00‰-4.00‰, and the corresponding average values in the stage Ⅲ were -108.00‰ (δDSMOW)and -1.89‰ (δ18OSMOW), meaning that magmatic derived solutions dominated in the early stages of mineralization, while meteoric water gradually played an important role in the later stage of mineralization. The sulfur isotope analysis showed that δ34S of pyrite was range of 1.50‰-4.20‰, indicating the metals mainly from deep-sourced magmas. All these lead to the conclusion that Baoxinggou gold deposit is of medium-low temperature magmatic hydrothermal origin which is directly related to the quartz diorite and diorite porphyritic magmatism.

Key words: Baoxinggou gold deposit, fluid inclusion, ore-forming fluid, ore genesis, Great Xing'an Range

CLC Number: 

  • P618.51
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