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WANG Gui, WANG Wei, WANG Gang, LI Tao, LIU Tao. 2021. Study on Multistage Uranium Mineralization of Hongshiquan Deposit in Longshoushan Metallogenic Belt. Northwestern Geology, 54(2): 157-165. doi: 10.19751/j.cnki.61-1149/p.2021.02.013
Citation: WANG Gui, WANG Wei, WANG Gang, LI Tao, LIU Tao. 2021. Study on Multistage Uranium Mineralization of Hongshiquan Deposit in Longshoushan Metallogenic Belt. Northwestern Geology, 54(2): 157-165. doi: 10.19751/j.cnki.61-1149/p.2021.02.013
shu

Study on Multistage Uranium Mineralization of Hongshiquan Deposit in Longshoushan Metallogenic Belt

  • No. 203 Research Institute of Nuclear Industry, Xianyang 712000, Shaanxi, China

Received Date:  22 June 2020
Revised Date:  12 October 2020
    Abstract
  • Hongshiquan deposit in Chinais the most typical uranium deposit of pegmatite type.In recent years,Hongshiquan deposit is found to have multi-stage uranium mineralization. Different ore,uranium minerals and alteration characteristics formed in different mineralization periods.Studies of different uranium mineralization show that in the late Zhongtiao period,granitic magma evolved into the light flesh red pegmatite granite ore rich in uraninite, with the ore concentrated in the core of the pegmatite granite, basically without alteration.In the Hercynian ore bearing hydrothermal solution, sodium metasomatic mineralization occurred along the contact fracture zone between the pegmatite granite and biotiteplagioschist,forming purple red pegmatite granite ore and asphalt uranium mineral.The ore develops albitization,hematite mineralization, carbonation, chloritization and other alteration.Therefore, the core of pegmatite granite and the contact fracture zone between pegmatite granite and schist are the important prospecting areas.
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    • References
  • 涂江汉.再谈红石泉铀矿床成因的若干问题[J].铀矿地质,1985,1(6):53-58.

    Google Scholar

    TU Jianghan.More Discussion About Some Problems on the Genesis of the Hongshiquan Uranium Deposit[J]. Uranium Geology,1985,1(6):53-58.

    Google Scholar

    张诚,金景福.红泉铀矿床含矿热液运移的数学模拟研究[J].矿床地质,1988,7(4):83-89.

    Google Scholar

    ZHANG Cheng,JIN Jingfu. A Mathematic Simulation Study on the Movement of Ore-bearing Hydrothermal Fluids in The Hongquan Uranium Ore Deposit[J]. Mineral Deposits,1988,7(4):83-89.

    Google Scholar

    张新虎.龙首山古裂谷带的基本特征及其演化历史[J].西北地质,1992,25(01):6-13.

    Google Scholar

    ZHANG Xinhu. Basic characteristics and evolution history of the Longshoushan ancient rift zone[J]. Northwestern Geology,1992,25(01):6-13.

    Google Scholar

    杜乐天.中国热液铀矿成矿理论体系[J].铀矿地质,2011,27(2):65-68+80.

    Google Scholar

    DU Letian. The Hydrothermal Alteration and Mineral Composition of Baixintu Uranium Deposit in Sonliao Basin[J]. Uranium Geology,2011,27(2):65-68+80.

    Google Scholar

    黄净白,黄世杰.中国铀资源区域成矿特征[J].铀矿地质,2005,25(3):129-138.

    Google Scholar

    HANG Jingbai,HUANG Shijie. Regional Metallogenic Characteristics of China's Uranium Resources[J]. Uranium Geology,2005,25(3):129-138.

    Google Scholar

    辛存林,马维云,安国堡,等.甘肃龙首山207铀矿床成矿地质特征及其成矿机制探讨[J].地质学报,2013,87(4):577-590.

    Google Scholar

    XIN Cunlin,MA Weiyun,AN Guobao,et al. Geological Characteristics and Mineralization Mechanism of the No. 207 Uranuim Deposit in Longshoushan, Cansu Province[J]. Acta Geologica Sinica,2013,87(4):577-590.

    Google Scholar

    尧宏福,张全傅.甘肃红石泉铀矿床晶质铀矿电子探针化学定年[J].世界有色金属,2017,(6):94-95.

    Google Scholar

    YAO Hongfu,ZHANG Quanfu. The Electron Microprobe Chemical Dating of Hongshiquan Pegmatitic Alaskite Uranium Deposit in Gusu Province[J]. World Nonferrous Metals,2017,(6):94-95.

    Google Scholar

    戎嘉树,韩泽宏,夏毓亮.我国一岩体型铀矿床的矿化特征及成矿作用[J].放射性地质,1984,(2):1-11.

    Google Scholar

    RONG Jiashu,HAN Zehong,XIA Yuliang. Mineralization characteristics and mineralization of one rock type uranium deposits in China[J]. Radiogeology,1984,(2):1-11.

    Google Scholar

    刘金枝,安伟涛.龙首山钠交代热液型铀矿床的碱交代作用研究[J].科技广场,2010,(7):187-189.

    Google Scholar

    LIU Jinzhi,AN Weitao. Study of Alkali Metasomatism on the Hydrothermal Uranium Deposit of Sodium Metasomatism in Longshou Mountain[J]. Science Mosaic, 2010,(7):187-189.

    Google Scholar

    赵如意,陈云杰,武彬,等.甘肃龙首山芨岭地区钠交代型铀矿成矿模式研究[J].地质与勘探,2013,49(01):67-74.

    Google Scholar

    ZHAO Ruyi,CHEN Yunjie,WU Bin,et al. A Metallogenic model of the Sodic-Metasomatic Type Uranium Ore Deposit in the Jiling area of Longshoushan,Gansu Province[J]. Geology and Exploration,2013,49 (01):67-74.

    Google Scholar

    张树明,魏正宇,张良,汤琳,赵新胤.龙首山碱交代型铀矿床特征和存在的问题[J].矿物学报,2013,33(S2):284-285.

    Google Scholar

    ZHANG Shuming,WEI Zhengyu,ZHANG Liang,et al. Characteristics and Existing Problems of the alkali-metasomatism uranium deposit in Longshoushan[J]. Acta Mineralogica Sinica,2013,33(S2):284-285.

    Google Scholar

    赵如意,王博,陈毓川,等.甘肃省龙首山牛角沟铀矿点钾钠混合交代作用研究[J].地质学报,2018,92(12):2469-2484.

    Google Scholar

    ZHAO Ruyi,Wang Bo,Chen Yuchuan,et al. On Potassium-sodium Mixed Metasomatism of the Niujiaogou Uranium Occurrence in Longshou Mountain,Gansu Province[J]. Acta Geologica Sinica,2018,92(12):2469-2484.

    Google Scholar

    刘正义,王生云,顾大钊,等.龙首山芨岭铀矿床含矿主岩特征及铀矿床成因讨论[J].西北地质,2018,51(02):160-170.

    Google Scholar

    LIU Zhengyi,WANG Shengyun,GU Dazhao,et al. Discussion on the Characteristics of Ore-bearing Rock and the Genesis of the Jiling Uranium Deposit[J]. Northwestern Geology,2018,51 (02):160-170.

    Google Scholar

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