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    Volume 30 Issue 2
    Mar.  2005
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    SHAO Fei, 2005. Low-Temperature Hot-Water in Xiangshan Orefield and Its Relation with Uranium Mineralization. Earth Science, 30(2): 206-210.
    Citation: SHAO Fei, 2005. Low-Temperature Hot-Water in Xiangshan Orefield and Its Relation with Uranium Mineralization. Earth Science, 30(2): 206-210.

    Low-Temperature Hot-Water in Xiangshan Orefield and Its Relation with Uranium Mineralization

    • Received Date: 2004-07-15
    • Publish Date: 2005-03-25
    • Xiangshan uranium orefield is one of the largest volcanic rock type hydrothermal uranium orefield in China. Beginning with modern warm hot-water in the orefield, and applying hydrogeochemistry and isotopic hydrogeology, this paper (analyzes) the geothermal characteristics of typical deposits, studies supply and heat sources of warm hot-water, and discusses the relation between hot-water and uranium mineralization according to the mechanism of uranium metallogenesis. The warm hot-water in Xiangshan orefield is hot-water of uplift fault type, meteoric water is the major supply source of warm hot- (water); deep circulation of groundwater and radioactive heat are the main channels for warm hot-water to obtain heat energy; hot-water activity made an important contribution to uranium metallogenesis; the uranium source mainly comes from water-rock interaction; a space unit is formed on integration with geothermal high field, warm hot-water and uranium mineralization which are controlled by base tectonics and volcano cover structure.

       

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