Volume 14 Issue 1
Mar.  2008
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SHAO Fei, CHEN Xiao-ming, XU Heng-li, et al., 2008. METALLOGENIC MODEL OF THE XIANGSHAN URANIUM ORE FIELD, JIANGXI PROVINCE. Journal of Geomechanics, 14 (1): 65-73.
Citation: SHAO Fei, CHEN Xiao-ming, XU Heng-li, et al., 2008. METALLOGENIC MODEL OF THE XIANGSHAN URANIUM ORE FIELD, JIANGXI PROVINCE. Journal of Geomechanics, 14 (1): 65-73.

METALLOGENIC MODEL OF THE XIANGSHAN URANIUM ORE FIELD, JIANGXI PROVINCE

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  • Received: 2007-07-12
  • Published: 2008-03-01
  • The authors studied the regional geological setting and metallogenic characteristics of the Xiangshan ore field and analyzed the sources of ore substances and ore fluids and channels for transport of ore substances, and on that basis, they constructed a uranium metallogenic model for the Xiangshan ore field. Uranium metallogenesis of the Xiangshan ore field took place in a specific temporal-spatial domain controlled by the regional geological setting; regional uranium-rich strata provided substances for metallogenesis; and ore fluids derived from magmatic water, mixed meteoric water, magma and postmagmatic hydrothermal fluids were carriers of uranium transport. The uranium metallogenic model emphasizes that the formation process of volcanic rocks was a process of ore substance concentration. The evolution of the volcanic postmagmatic hydrothermal ore system gave birth to ore-forming processes with a time span of 50 Ma in the Xiangshan volcanic basin. The coupling of metallogenic mechanisms such as temperature decline, concentration and mixing of fluids promoted uranium precipitation and ore formation.

     

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  • [1]
    Chen Zhaobo." Double mixing" genetic model of uranium deposits in volcanic rocks and relationship between China's Mesozoic veintype uranium deposits and Pacific plate tectonics, M etallogensis of Uranium[J].In:Proceedings of the 26th IGC, Geoinstitute, Beogard, 1981, 65~97.
    [2]
    李学礼, 孙占学, 周文斌.古水热系统与铀成矿作用[M].北京:地质出版社, 2000.
    [3]
    杜乐天.中国热液铀矿基本成矿规律和一般热液成矿学[M].北京:原子能出版社, 2001.
    [4]
    张勤文, 黄怀曾.中国东部中、新生代构造-岩浆活化史[J].地质学报, 1982, 2:111~122. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000377655
    [5]
    王德滋, 杜杨松.东南沿海地区中生代火山-侵入杂岩形成的构造背景[J].矿物岩石地球化学通讯, 1990, 3:186 ~188. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000002008654
    [6]
    邱爱金.江西相山铀矿田东西向隐伏构造的发现及其地质意义[J].地质论评, 2001, 47 (6):637 ~641. doi: 10.3321/j.issn:0371-5736.2001.06.012
    [7]
    黄志章, 李秀珍, 蔡根庆.热液铀矿床蚀变场及蚀变类型[M].北京:原子能出版社, 1999.
    [8]
    夏林圻, 夏祖春, 张成, 等.相山中生代含铀火山杂岩岩石地球化学[M].北京:地质出版社, 1992.
    [9]
    章邦桐, 张祖还, 倪奇生.内生铀矿床及其研究方法[M].北京:原子能出版社, 1990.
    [10]
    江西省地质矿产局.江西省区域地质志[M].北京:地质出版社, 1984.
    [11]
    沈渭洲.同位素地质学教程[M].北京:原子能出版社, 1997.
    [12]
    张理刚, 陈振胜, 刘敬秀, 等.两阶段水-岩同位素交换理论及其勘查应用[M].北京:地质出版社, 1995.
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