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| Geological Characteristics and Genesis of the ShuiyindongGold Deposit, Guizhou |
| QI Shao-feng1, CHEN Fa-en2, FENG Lin1, SHI Yi1 |
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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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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Received: 22 April 2015
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2015, Vol. 2 
