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Geoscience ›› 2021, Vol. 35 ›› Issue (06): 1523-1535.DOI: 10.19657/j.geoscience.1000-8527.2021.127

• Gold-polymetallic Mineralization in Qinling Orogens • Previous Articles     Next Articles

Geological Characteristics and Genesis of the Xiangtanzi Gold Deposit in Liangdang County, Gansu Province

GAO Yinhu1(), YIN Gang1, GONG Zeqiang2, GUO Mingchun3   

  1. 1. The First Institute of Geology and Mineral Exploration, Gansu Bureau of Geology and Mineral Exploration and Development, Tianshui, Gansu 741020, China
    2. Liangdang Zhaojin Gold Industry Co., Ltd.,Liangdang,Gansu 742400,China
    3. Zhejiang Geological Exploration Institute of China Metallurgical Geology Administration,Quzhou,Zhejiang 324000,China
  • Received:2021-10-20 Revised:2021-11-05 Online:2021-12-10 Published:2022-02-14

Abstract:

The Xiangtanzi gold deposit is located in the eastern West Qinling orogenic belt. The gold deposit is mainly controlled by NW-trending faults, and is closely related to the local intermediate-felsic dikes. Microscopic observation and electron microprobe analysis show that Au is mainly hosted in pyrite and arsenopyrite. The Co/Ni characteristics of pyrite in the ore body show that the genesis of pyrite is related to magmatism. Through REE analysis, it is found that REE characteristics of ore are basically consistent with those of rock mass, but obviously different from those of surrounding rock.The sulfur isotope of pyrite in the ore was tested and the ore sulfide δ34S values are from -5.7‰ to 2.0‰ (avg.0.38‰), clustering around zero with a tower distribution, which indicates that the ore sulfur source is magmatic. By hydrogen and oxygen isotope analysis, the Xiangtanzi gold ore has δ18${{\text{O}}_{{{\text{H}}_{2}}\text{O}}}$=3.44‰-9.65‰ (avg.6.29‰) and δD=-120.10‰ to -79.00‰ (avg.-100.47‰). This indicates that the ore-forming fluid in this area came mainly from magmatic water.Pb isotope characteristics indicates that the Pb evolution at Xiangtanzi was closely related to magmatism and orogeny. A comparative study shows that the metallogenic epoch of the Xiangtanzi gold deposit is late Indosinian. The Xiangtanzi gold deposit is a vein shaped ore body controlled by shallow fault system, which was invaded by magma containing ore-forming materials and fluids in the late Indosinian period. The discovery and genesis of Xiangtanzi gold deposit is of great significance to the prospecting direction in West Qinling area.

Key words: West Qinling orogenic belt, Xiangtanzi gold deposit, geological characteristic, geochemical characteristic, ore genesis

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