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《China Tungsten Industry》 2009-05
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Xiaodushanxi Tungsten Deposit' s Mineralization Mechanism

CHEN Yu-feng 1 , DONG Yin-feng2, XIAO Ze-zhong1 (1. No.4. Team of Non-ferrous Geological Prospecting Bureau of Gansu, Zhangye 734012, Gansu, China; 2. The fourth Geology and Mineral Exploration Academy of Shandong, Weifang 261021, Shandong, China)  
This paper discusses the mineralization mechanism of the large-scaled Xiaodushanxi tungsten deposit from the conditions of stratigraphy, tectonics, magmatic rocks and wall-rocks alteration. The above conditions perfect coupling is the fundamental reason for the formation of this deposit. Material condition provides by Lower Permian Hongliuhe group lithology layer for its high tungsten value. Extremely fractured fault systems provide the channel for migration of the later ore-forming hydrothermal, and provide the access and storage space for ore-forming material exchange, sediment-rich and mineralization. Yanshan early magmatic activity provide heat and material sources, at the same time, the early fracture systems' re-activities provide a wider channel and storage space for the hydrothermal migration, material exchange, mineralization. Yanshan early post -magmatic hydrothermal filled and exchanged along the pre-formed account of fractures. In the periods quartz-type wolfram formed under high-temperature phase, and quartz-type scheelite formed with the gradual lowering of temperature. After formation of the deposit, placer tungsten formed along the valley by weathering for a long time. So the deposit is a filling-replacement wolfram and scheelite deposit related to acidic magma. Searching for ore-forming hydrothermal migration pathway and its direction will become the working focus in the future prospecting in this area.
【CateGory Index】: P618.67
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