Volume 28 Issue 3
Jun.  2022
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Article Navigation >  Journal of Geomechanics  > 2022  >  28(3): 448-463
MIN Zhuang, CHEN Zhengle, PAN Jiayong, et al., 2022. Research on fluid inclusions of the Jiadi gold deposit in southwestern Guizhou. Journal of Geomechanics, 28 (3): 448-463. DOI: 10.12090/j.issn.1006-6616.2021170
Citation: MIN Zhuang, CHEN Zhengle, PAN Jiayong, et al., 2022. Research on fluid inclusions of the Jiadi gold deposit in southwestern Guizhou. Journal of Geomechanics, 28 (3): 448-463. DOI: 10.12090/j.issn.1006-6616.2021170
shu

Research on fluid inclusions of the Jiadi gold deposit in southwestern Guizhou

doi: 10.12090/j.issn.1006-6616.2021170
  • 1.

    School of Earth Sciences, East China University of Technology, Nanchang 330013, Jiangxi, China

  • 2.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 3.

    Beijing Research Institute of Uranium Geology, CNNC, Beijing 100029, China

  • 4.

    Research Institute No. 270, CNNC, Nanchang 330299, Jiangxi, China

Funds:

the Science and Technology Project of Guizhou Province 2021-408

Geological Survey Projects of the China Geological Survey DD20190161

Geological Survey Projects of the China Geological Survey DD20221660-3

Guizhou Carlin-type Gold Deposit Metallogenic and Prospecting Scientific and Technological Innovation Talent Team Construction Project CXTD2021-007

China Uranium Industry Corporation-East China University of Technology Joint Innovation Fund Project NRE2021-01

Open Fund Project of State Key Laboratory of Nuclear Resources and Environment of East China University of Technology 2020NRE04

More Information
  • Received: 2021-12-21
  • Revised: 2022-05-09
    Abstract
  • The Jiadi gold deposit, located in southwestern Guizhou Province, is a newly discovered large-scale basalt-hosted and fine-grained disseminated gold deposit. This article focuses on the characteristics of ore-forming fluid in order to discuss the ore-forming mechanism by the fluid inclusion analyses from different mineralization stages of the deposit. Based on the field observations and laboratory analyses, the hydrothermal ore-forming processes of the deposit can be divided into three stages: the pyritization forming-stage (1st stage), the smoky-gray quartz forming-stage (2nd stage) and the sulfide forming-stage (3rd stage), among which the smoky-gray quartz forming-stage is the primary stage. The fluid inclusions are mainly composed of NaCl-H2O and CO2-NaCl-H2O type, and CO2-rich inclusions are frequently observed in the first stage minerals, with homogenization temperature (Th) ranging from 211 to 231℃, and salinity (wt) from 2.10 to 7.60 (%NaCl equiv). There are a lot of NaCl-H2O and CO2-NaCl-H2O type of inclusions in the second stage, with the homogenization temperature (Th) changing from 182 to 218℃, and the salinity (wt) from 1.40 to 5.90 (%NaCl equiv). The homogenization temperature (Th) of the third stage is generally lower than 183℃, with the salinity (wt) varying from 0.90 to 5.30 (%NaCl equiv). The results of laser Raman spectroscopy show that the inclusions generally contain CO2, CH4, N2, SO2 and other gas-phase components. As the homogeneous temperature, salinity and density of the ore-forming fluid continue to decrease, the component types in the inclusions tend to reduce. By calculating the ρ, P, pH, Eh, and ƒO2, the ore-forming environment is characterized by low to moderate temperatures, low salinity, low density, near neutrality, relative reducibility and low oxygen fugacity. The change in fluid inclusion assemblage (FIA) indicates that the mineralization occurred as the fluid CO2 content continued to decrease. The fluid mixing in the main ore-forming stage and the regional extensional structure caused strong fluid boiling, and a large number of metal components (pyrite, natural gold, etc.) were rapidly precipitated to form gold ore bodies.

     

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