胶东牟乳成矿带范家庄金矿床成矿流体特征及其地质意义

doi:10.13278/j.cnki.jjuese.20180339

Abstract

Abstract: The Muping-Rushan metallogenic belt is one of the three major gold metallogenic belts in the world-class Jiaodong gold province. However, its sources of ore-forming fluids is still hotly debated. The Fanjiazhuang deposit is a newly discovered gold deposit in this belt, and the study of its ore-forming fluid is relatively weak. Combined with the geological characteristics of the deposit, the fluid inclusions,hydrogen, and oxygen isotopic geochemistry were analyzed to understand the characteristics, origin, and evolution of the ore-forming fluids. The gold orebodies are mainly existed in Jurassic granites, in vein and lens shape, and are controlled obviously by fault structures. The hydrothermal mineralization of Fanjiazhuang deposit can be divided into 3 stages: Quartz-coarse pyrite (early metallogenic stage), quartz-Au polymetallic sulfide (major metallogenic stage), and quartz-carbonate (late metallogenic stage). The petrographic observation indicates that there are mainly two-phase aqueous and mono-phase liquid aqueous inclusions, with a few three-phase CO₂-bearing inclusions. The micro-thermometry shows that the homogeneous temperature of the fluid inclusions in the early and major metallogenic stages is 167.2-297.5 ℃ and 168.4-253.6 ℃, salinity is 3.55%-22.65% and 2.58%-12.05%, and density is 0.77-1.06 g/cm³ and 0.84-1.02 g/cm³, respectively. All these features indicate the characteristics of middle-low temperature, middle-low salinity, and low density, a typical mesothermal gold deposit. The ore-forming pressure in the major metallogenic stage is estimated to be 45.8-68.7 MPa (average 52.8 MPa), and the corresponding ore-forming depth is 5.38-6.71 km (average 5.93 km), medium-shallow mineralization. The hydrogen and oxygen isotopic compositions of the ore-forming fluids show the δD_H₂O-SMOW value from -96.9‰ to -89.0‰ and the δ¹⁸O_H₂O-SMOW value from -4.3‰ to 4.5‰ in the early stage. The δD_H₂O-SMOW and δ¹⁸O_H₂O-SMOW values in the major metallogenic stage change from -90.7‰ to -85.3‰ and from -5.4‰ to -0.2‰, respectively. All these above suggest that the ore-forming fluid of Fanjiazhuang gold deposit was derived from the mixture of magmatic water and meteoric water, and the proportion of the latter increased with the evolution of the ore-forming fluid. Based on the geological and fluid inclusion features, Fanjiazhuang deposit should be a mesothermal gold deposit.

Key words: fluid inclusions, hydrogen and oxygen isotopes, mesothermal gold deposit, Fanjiazhuang gold deposit, Muping-Rushan metallogenic belt

CLC Number:

P618.51

Wang Yongjun, Liu Yan, Huang Xin, Xu Chang, Shen Lijun, Zhang Yezhi, Zhang Zhaomin. Characteristics of Ore-Forming Fluids and Geological Significance of Fanjiazhuang Gold Deposit in Muping-Rushan Metallogenic Belt, Jiaodong Peninsula[J].Journal of Jilin University(Earth Science Edition), 2020, 50(4): 1012-1028.

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