Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (6): 1717-1731.doi: 10.13278/j.cnki.jjuese.201706111

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Fluid Inclusion of Yaojiagou Porphyry Mo Deposit in Qingchengzi in Liaoning Province

He Chengzhong1,2, Zhang Dehui1, Wu Mingqian1, Xia Yan3, Zhang Rongzhen1,4, Hu Tiejun5   

  1. 1. School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China;
    2. No.10 Gold Geological Party of CAPF, Kunming 650111, China;
    3. Qingchengzi Mining Co., Ltd., Fengcheng 118100, Liaoning, China;
    4. Henan Institute of Geological Survey, Zhengzhou 450001, China;
    5. Nonferrous Geological Bureau Exploration Institute of Liaoning Province, Shenyang 110000, China
  • Received:2017-03-22 Online:2017-11-26 Published:2017-11-26
  • Supported by:
    Supported by the National Natural Science Foundation of China(41373048) and Public Welfare Industry Research of Ministry of Land and Resources(201411024)

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Abstract: The Yaojiagou molybdenum deposit is a newly discovered one in recent years in the ore field of Qingchengzi in Liaoning. It is located in the Yan-Liao Mo metallogenic belt in the northern margin of the North China craton. The quartz veins (UST)and quartz eyes in the Yaojiagou pluton are direct evidence of fluid exsolution from magma. Deposit alteration zonation is significant,and the molybdenum mineralization mainly exists in the potassic and skarn zones. After a microscopic observation,we found various abundant fluid inclusions,including single-phase aqueous (PW-type), two-phase aqueous (W-type), three-phase CO2 (C-type), pure CO2 (PC-type),and daughter mineral-bearing inclusions (S-type) in which the daughter minerals are hematite, chalcopyrite,and some other unknown minerals with no halite. The fluid evolution in this deposit are:1) the early quartz eye stage with the homogenization temperature of 211.4-515.4℃, salinity of 0.8%-19.2%,and rich in CO2; 2) the quartz veins mineralization stage with the homogenization temperature of 179.5-424.5℃ and salinity of 2.4%-21.5% in NaCl-H2O-CO2 system;3) the late quartz veins stage with the homogenization temperature of 167.8-353.3℃ and salinity of 3.4%-15.8% in NaCl-H2O-CO2 system;4) the latest calcite veins stage with the homogenization temperature of 132.5-234.1℃ and salinity of 0.9%-11.2% in NaCl-H2O system;5)the UST quartz veins stage with the homogenization temperature of 158.6-381.7℃ and salinity of 1.6%-21.5% in NaCl-H2O-CO2 system, and this stage represents a immiscible fluid exsolution from a shallower intrusive magma with no mineralization. Wall rock alteration and fluid mixing are the main mechanisms of ore-forming metal elements precipitation,which lead to fluid temperature, pressure reduction, CO2 escaping,and system rebalancing. We obtained the capture pressure of 124-180 MPa with the corresponding depth of 4.6-7.0 km during the ore-forming period by using the method of isochore intersection. It is relatively deeper than that of the other molybdenum deposits in the northern margin of the North China craton.

Key words: Yaojiagou Mo deposit, porphyry deposit, fluid inclusion, fluid's characteristics, metallogenic depths, Qingchengzi ore field

CLC Number: 

  • P618.65
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