中国地质调查局西安地质调查中心主办
高级检索

广西油麻坡钨钼矿床流体包裹体与成因探讨

,  ,  ,  ,  , 

文章导航 > 西北地质 > 2017 > 50(2): 178-190

上一篇

下一篇

张文兵, 蔡明海, 李强, 薛彦萍, 刘翔, 郑浩. 广西油麻坡钨钼矿床流体包裹体与成因探讨[J]. 西北地质, 2017, 50(2): 178-190.
引用本文: 张文兵, 蔡明海, 李强, 薛彦萍, 刘翔, 郑浩. 广西油麻坡钨钼矿床流体包裹体与成因探讨[J]. 西北地质, 2017, 50(2): 178-190.
shu
ZHANG Wenbing, CAI Minghai, LI Qiang, XUE Yanping, LIU Xiang, ZHANG Hao. Fluid Inclusion Study and Genesis of the Youmapo W-Mo Deposit in Guangxi Province[J]. Northwestern Geology, 2017, 50(2): 178-190.
Citation: ZHANG Wenbing, CAI Minghai, LI Qiang, XUE Yanping, LIU Xiang, ZHANG Hao. Fluid Inclusion Study and Genesis of the Youmapo W-Mo Deposit in Guangxi Province[J]. Northwestern Geology, 2017, 50(2): 178-190.
shu

广西油麻坡钨钼矿床流体包裹体与成因探讨

  • 广西大学资源与冶金学院, 广西 南宁 530004

  • 基金项目: 广西钨钼典型矿床专题研究、广西壮族自治区钨钼成矿规律研究（桂财建函[2015]118号）

Fluid Inclusion Study and Genesis of the Youmapo W-Mo Deposit in Guangxi Province

  • College of Resource and Metallurgy, Guangxi University, Nanning 530004, Guangxi, China

    摘要
  • 油麻坡钨钼矿床是桂东南博白-岑溪W-Mo-Pb-Zn-Au-Ag成矿带内新近评价的一个大型矽卡岩型矿床，矿体产于泥盆系下统矽卡岩中。将成矿划分为干矽卡岩阶段（Ⅰ）、湿矽卡岩阶段（Ⅱ）、石英-硫化物阶段（Ⅲ）和碳酸盐-萤石阶段（Ⅳ），其中，Ⅱ和Ⅲ为主成矿阶段。为探究成矿作用中成矿流体特征，采用流体包裹体显微测温对主成矿阶段流体的性质进行了研究。研究表明，Ⅱ阶段即湿矽卡岩阶段流体包裹体均一温度主要集中于280~340℃，盐度主要集中于3.33%~5.94%；Ⅲ阶段即石英-硫化物阶段流体包裹体均一温度主要集中于260~320℃，盐度主要集中于5.05%~9.99%。成矿流体以中高温、低盐度为特征。成矿过程中流体发生过沸腾和混合作用。区内成矿与燕山晚期油麻坡岩体有关，属中高温岩浆热液交代-充填型矿床。
    Occurred in the Lower Devonian skarn, the Youmapo tungsten-molybdenum deposit is a large-size recently evaluated skarn type deposit in the Bobai-Cenxi W-Mo-Pb-Sn-Au-Ag metallogenic belt, southeast Guangxi.Four stages of skarn-type ores have been distinguished, i.e., Stage Ⅰ-dry skarn stage, Stage Ⅱ-wet skarn stage, Stage Ⅲ-quartz and sulfide stage, and Stage Ⅳ-carbonate and fluorite stage.In addition, the Stage Ⅱ and the Stage Ⅲ are main metallogenic stages.In order to explore the characteristics of ore-forming fluid in mineralization, the microthermometry of fluid inclusions has been used to research the nature of the ore-forming fluids in the main ore-forming stage.Results indicate that the homogenization temperatures of the fluid inclusions in stage Ⅱ and Ⅲ mainly vary from 280 to 340℃ and from 260 to 320℃, whereas their salinities mainly range from 3.33% to 5.94% and from 5.05% to 9.99%, respectively.The ore-forming fluid in this deposit has the characteristics of medium to high homogenization temperatures and low salinity.Boiling and mixing have occurred during the mineralization.The ore deposit is a medium to high magmatic hydrothermal replacement filling type deposit, and the mineralization in the area was related to late Yanshanian Youmapo pluton.
    • HTML全文
  • 加载中
    • 参考文献(55)

  • 毛伟.广西东部金银成矿特征及找矿方向[J].广西地质, 1995, 8(2):37-54.

    MAO Wei.Metallogenetic laws and exploration prospects of Au and Ag deposits in eastern Guangxi[J].Guangxi Geology, 1995, 8(2):37-54 (in Chinese with English abstract).

    冯佐海,雷良奇,张起钻,等.佛子冲铅锌矿田火山岩覆盖区构造控矿特征[J].有色金属矿产与勘查, 1999, 8(6):423-427.

    FENG Zuohai, LEI Liangqi, ZHANG Qizuan, et al.The ore-controlling structures in the volcanics-covered Area, Fuzichong Area, Pb-Zn ore field, Guangxi[J].Geological Exploration For Non-Ferroos Metals, 1999, 8(6):423-427 (in Chinese with English abstract).

    杨斌,李骏青.广西东桃铅锌矿床喷流-沉积地球化学特征[J].矿产与地质, 2000, 14(5):333-336.

    YANG Bin, LI Junqing.Exhalative-sedimentary geochemical features of Guangxi DongTao Lead-Zinc deposit[J]. Mineral Resources and Geology, 2000, 14(5):333-336 (in Chinese with English abstract).

    杨斌,刘建明,李水如.广西佛子冲铅锌矿田热水沉积绿色岩和碳酸盐岩建造[J].矿床地质, 2002, (S1):1068-1071.

    YANG Bin, LIU Jianming, LI Shuiru.Green-rock and carbonate construction formed by hot-water sedimentation in fozichong Lead-Zinc ore field[J].Mineral Deposits, 2002, (S1):1068-1071 (in Chinese with English abstract).

    雷良奇,宋慈安,冯佐海.广西佛子冲铅锌(银)成矿带多元素富集特征及矿床成因[J].矿床地质, 2002, 21(1):74-82.

    LEI Liangqi, SONG Cian, FENG Zuohai.Discussion on multi-element enrichment characteristics and genesis of Fuzichong Pb-Zn(Ag) Metallogenic Belt, Guangxi[J]. Mineral Deposits, 2002, 21(1):74-82 (in Chinese with English abstract).

    黄惠兰,蔡明海,彭松柏,等.广西东桃铅锌矿床流体包裹体研究[J].地质科技情报, 2004, 23(2):31-35.

    HUANG Huilan, CAI Minghai, PENG Songbai, et al.Fluid inclusion of DongTao Lead-Zinc deposit in Guangxi[J]. Geological Science and Technology Information, 2004, 23(2):31-35 (in Chinese with English abstract).

    李金发,蔡明海.广西东桃铅锌矿床控矿构造特征及其同位素年代学研究[J].地质科技情报, 2004, 23(2):63-67.

    LI Jinfa, CAI Minghai.Ore-controlling structure festures and isotopic geochronology of DongTao Lead-Zinc deposit in Guangxi[J].Geological Science and Technology Information, 2004, 23(2):63-67 (in Chinese with English abstract).

    蔡锦辉,韦昌山,王猛,等.广西佛子冲铅锌矿田地质特征及找矿模式[J].华南地质与矿产, 2007, (3):12-23.

    CAI Jinhui, WEI Changshan, WANG Meng, et al.The geological characteristics and prospecting mode of the Fuzichong Pb-Zn ore field, Guangxi[J].Geology and Mineral Resources of South China, 2007, (3):12-23 (in Chinese with English abstract).

    翟丽娜,王建辉,韦昌山,等.广西佛子冲铅锌矿田成岩成矿时代研究[J].华南地质与矿产, 2008, (3):46-49.

    ZHAI Lina, WANG Jianhui, WEI Changshan, et al.Researching on the age of rock-forming and metallogenic epoch of Fuzichong ore field in Guangxi[J]. Geology and Mineral Resources of South China, 2008, (3):46-49 (in Chinese with English abstract).

    刘贤才.广西博白中苏银金矿特征及成因探讨[J].科技创新导报, 2011, (18):115.

    LIU Xiancai.Disscusion on characteristics and genesis of Zhongsu Ag-Au deposit in Bobai, Guangxi[J].Science and Technology Innovation Herald, 2011, (18):115 (in Chinese).

    韦龙明,冯经平,付伟,等.广西佛子冲铅锌矿绿色岩REE地球化学特征及成矿指示意义[J].桂林理工大学学报, 2012, 32(2):155-161.

    WEI Longming, FENG Jingping, FU Wei, et al.REE geochemical characteristics of green rock in Fozichong Lead-Zinc deposit and genesis implications[J].Journal of Guilin University of Technology, 2012, 32(2):155-161 (in Chinese with English abstract).

    付伟,柴明春,杨启军,等.广西佛子冲大型铅锌多金属矿床的成因:流体包裹体和H-O-S-Pb同位素地球化学约束[J].岩石学报, 2013, 29(12):4136-4150.

    FU Wei, CHAI Mingchun, YANG Qijun, et al.Genesis of the Fozichong Pb-Zn polymetallic deposit:constraints from fluid inclusions and H-O-S-Pb isotopic evidences[J].Acta Petrologica Sinica, 2013, 29(12):4136-4150 (in Chinese with English abstract).

    付强,葛文胜,温长顺,等.广西油麻坡钨钼矿床地质特征及成因探讨[J].矿床地质, 2010, S1:183-184.

    FU Qiang, GE Wensheng, WEN Changshun, et al.Geologic feature and genesis of Youmapo W-Mo deposit in Guangxi[J].Mineral Deposits, 2010, S1:183-184 (in Chinese with English abstract).

    杨拓.广西博白油麻坡钨钼矿床地质特征及找矿标志[J].矿产与地质, 2013, 27(5):381-387.

    YANG Tuo.Geological characteristics and clues fro prospecting of Youmapo W-Mo deposit in Bobai of Guangxi[J].Mineral Resources and Geology, 2013, 27(5):381-387 (in Chinese with English abstract).

    王炯辉,马星华,李毅,等. 花岗质复式岩体成因及其与W-Mo成矿的关系——以广西油麻坡岩体为例[J].地质学报, 2014, 88(7):636-658.

    WANG Jionghui, MA Xinghua, LI Yi, et al.Petrogenesis of granitic complexes and implications for the W-Mo mineralization:a case study from the YOumapo pluton, Guangxi Province[J].Acta Geologica Sinca, 2014, 88(7):636-658 (in Chinese with English abstract).

    付强,葛文胜,温长顺,等.广西油麻坡钨钼矿床地球化学特征及成因探讨[J].矿床地质, 2014, 33(4):785-794.

    FU Qiang, GE Wensheng, WEN Changshun, et al.Geochemistry and genesis of Youmapo W-Mo deposit in Guangxi[J].Mineral Deposits, 2014, 33(4):785-794 (in Chinese with English abstract).

    冯定素,毛景文,陈懋弘,等.广西油麻坡钨钼矿床成岩成矿年代学研究及其地质意义[J].矿床地质, 2016, 35(3):491-508.

    FENG Dingsu, MAO Jingwen, CHEN Maohong, et al.Geochronology of Youmapo W-Mo deposit in Guangxi and its geological significance[J].Mineral Deposit, 2016, 35(3):491-508 (in Chinese with English abstract).

    周永章,郑义,曾长育,等.关于钦-杭成矿带的若干认识[J].地学前缘, 2015, 22(2):1-6.

    ZHOU Yongzhang, ZHENG Yi, ZENG Changyu, et al.On the understanding of Qinzhou Bay-Hangzhou Bay metallogenic belt, South China[J].Earth Science Frontiers, 2015, 22(2):1-6 (in Chinese with English abstract).

    罗璋.广西博白-岑溪断裂带地质特征与构造演化[J].广西地质, 1990, 3(1):25-34.

    LUO Zhang.The geological features and tectnotic evolution in Bobai-Cenxi deep fault zone,Guangxi[J].Geology of Guangxi, 1990, 3(1):25-34 (in Chinese with English abstract).

    广西壮族自治区地质勘查总院.广西钼矿资源潜力评价报告[R].2012.

    卢焕章,范宏瑞,倪培,等.流体包裹体[M].北京:科学出版社:2004.

    LU Huanzhang, FAN Hongrui, NI Pei, et al.Fluid inclusion[M].Beijing:Science Press, 2004 (in Chinese).

    刘斌,沈昆.流体包裹体热力学[M].北京:地质出版社:1999.

    LIU Bin, SHEN Kun.Fluid inclusion thermodynamics[M].Beijing:Geology Press, 1999 (in Chinese).

    龚庆杰.地质流体的热力学与化学动力学分析及其应用研究[D].中国地质科学研究院矿产资源研究所, 2005.

    GONG Qingjie.Thermodynamics and chemical kinetics analysis of geological fluid and its application[D].Institute of Mineral Resources, Chinese Academy of Geological Science, 2005 (in Chinese).

    冷成彪,张兴春,王守旭,等.岩浆-热液体系成矿流体演化及其金属元素气相迁移研究进展[J].地质论评, 2009, 55(1):100-112.

    LENG Chengbiao, ZHANG Xingchun, WANG Shouxu, et al.Advances of researches on the evolution of ore-forming fluids and the vapor transport of metals in Magmatic-hydrothermal systems[J].Geological Review, 2009, 55(1):100-112 (in Chinese with English abstract).

    蔡建明,刘若兰,曾广胜.江西盘古山钨矿包裹体含盐度和CO2成分的研究及其在成矿中的意义[J].成都地质学院学报, 1981, (2):99-103.

    CAI Jianming, LIU Ruolan, ZENG Guangsheng.Researches on the salinity and CO2 componenes from Tungsten fluid inclusions and its significance of mineralization in PanGushan, Jiangxi[J].Journal of Chengdu Institute of Geology, 1981, (2):99-103 (in Chinese).

    张文淮,张志坚,伍刚.成矿流体及成矿机制[J].地学前缘, 1996, 3(4):245-252.

    ZHANG Wenhuai, ZHANG Zhigang, WU Gang.Ore-forming fluid and mineralization mechanism[J].Earth Science Frontiers, 1996, 3(4):245-252 (in Chinese with English abstract).

    池国祥,薛春纪.成矿流体动力学的原理、研究方法及应用[J].地学前缘, 2011, 18(5):1-18.

    CHI Guoxiang, XUE Chunji.Principles, methods and applications of hrdrodynamic studies of mineralization[J].Earth Science Frontiers, 2011, 18(5):1-18 (in Chinese with English abstract).

    ROEDDER E.Fluid inclusions[J].Reviews in Mineralogy, 1984, (12):25-35.

    DIAMOND L W.Review of the systematics of CO2-H2O fluid inclusions[J].Lithos, 2001, (55):69-99.

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  2837
  • PDF下载数:  2017
  • 施引文献:  0
出版历程
收稿日期:  2017-01-16
修回日期:  2017-02-15
刊出日期:  2017-06-15

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回