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QI Shao-feng, CHEN Fa-en, FENG Lin, et al. Geological Characteristics and Genesis of the ShuiyindongGold Deposit, Guizhou[J]. Geological Survey of China, 2015, 2(6): 53-58.
Citation: QI Shao-feng, CHEN Fa-en, FENG Lin, et al. Geological Characteristics and Genesis of the ShuiyindongGold Deposit, Guizhou[J]. Geological Survey of China, 2015, 2(6): 53-58.
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Geological Characteristics and Genesis of the ShuiyindongGold Deposit, Guizhou

  • 1.

    Geological Archives of Guizhou Province, Guiyang, Guizhou 550002, China

  • 2.

    The 105th Geological Team, Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang, Guizhou 550018, China

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  • Received Date: April 21, 2015
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    • Abstract
  • The Shuiyindong gold deposit is a typical carlin type gold deposit in the contiguous areas of Yunnan-Guizhou-Guangxi provinces. The gold ore-bodies are controlled by fault structures within anticlinal axis, and distributed in an unconformity interface between Longtan Formation (P3l) and Maokou Formation (P2m) of Permian Period. The wave-shaped ore-bodies eastwardly plunged in strike direction, and spatially overlapped in vertical direction. It is suggested that the Shuiyindong gold deposit is a carlin type gold deposit which occurred in structural alteration zone of sedimentary carbonate rocks, and is controlled by fault-hydrothermal system. The ore-forming environment is characterized by epithermal, high pressure.
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    • References (4)
  • [1]
    冯琳,张竹如.泥堡金矿与水银洞金矿地质特征初步对比[J].贵州地质, 2005,22(1):22-25.
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    聂爱国,张竹如.黔西南水银洞金矿床成矿地质条件研究[J].黄金,2006,27(6):5-9.
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    王砚耕.黔西南构造与卡林型金矿[M].北京:地质出版社,1994.
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