中国地质调查局西安地质调查中心主办
高级检索

喀喇昆仑地区豹子山铅锌矿地质特征与成因浅析

,  ,  ,  , 

文章导航 > 西北地质 > 2020 > 53(2): 172-182

上一篇

下一篇

高峰, 菅坤坤, 张振凯, 潘亮, 杜彪. 2020. 喀喇昆仑地区豹子山铅锌矿地质特征与成因浅析. 西北地质, 53(2): 172-182. doi: 10.19751/j.cnki.61-1149/p.2020.02.010
引用本文: 高峰, 菅坤坤, 张振凯, 潘亮, 杜彪. 2020. 喀喇昆仑地区豹子山铅锌矿地质特征与成因浅析. 西北地质, 53(2): 172-182. doi: 10.19751/j.cnki.61-1149/p.2020.02.010
shu
GAO Feng, JIAN Kunkun, ZHANG Zhenkai, PAN Liang, DU Biao. 2020. Geological Characteristics and Genesis Analysis of Baozishan Pb-Zn Deposit in Karakoram Area. Northwestern Geology, 53(2): 172-182. doi: 10.19751/j.cnki.61-1149/p.2020.02.010
Citation: GAO Feng, JIAN Kunkun, ZHANG Zhenkai, PAN Liang, DU Biao. 2020. Geological Characteristics and Genesis Analysis of Baozishan Pb-Zn Deposit in Karakoram Area. Northwestern Geology, 53(2): 172-182. doi: 10.19751/j.cnki.61-1149/p.2020.02.010
shu

喀喇昆仑地区豹子山铅锌矿地质特征与成因浅析

  • 1. 陕西省地质调查院, 陕西 西安 710054;

  • 2. 长安大学, 陕西 西安 710054

  • 基金项目:

    国家专项“第二次青藏高原综合科学考察研究”（2019QZKK0806），中国地质调查局“新疆河尾滩—河西岗地区1∶5万矿产地质调查”项目（DD20160004-5）

详细信息
    作者简介: 高峰(1985-),男,在职研究生,高级工程师,长期从事区域地质调查和矿产勘查工作。E-mail:gaofengddzx@163.com

  • 中图分类号: P618.42;P618.43

Geological Characteristics and Genesis Analysis of Baozishan Pb-Zn Deposit in Karakoram Area

  • 1. Shaanxi Institute of Geological Survey, Xi'an 710054, Shaanxi, China;

  • 2. Chang'an University, Xi'an 710054, Shaanxi, China

    摘要
  • 新疆和田地区豹子山铅锌矿具与热液交代作用有关的后生矿床的地质特征，矿化赋存于中侏罗统龙山组碳酸盐岩中，严格受北西向断裂构造控制，矿石矿物组分简单，主要矿物为菱锌矿和白铅矿，围岩蚀变以赤铁矿化、褐铁矿化为主。矿石S同位素组成分布范围较宽（δ34S=-8.49‰~24.88‰），S具多源性，主要源于沉积岩地层，有地表流体的加入；矿石Pb同位素组成较均一，206Pb/204Pb=18.807~18.822，207Pb/204Pb=15.73~15.756，208Pb/204Pb=39.055~39.168，μ=9.68~9.73，Pb源于上地壳；矿石δ13CV-PDB=2.85‰~8.25‰，δ18OV-SMOW=20.04‰~21.07‰，C、O来源于碳酸盐岩，而非岩浆热液。综合矿床地质及同位素特征，认为其成因类型属构造热液-直接交代型铅锌矿。
    The lead-zinc deposit of Baozishan,which is located in the Hetian area of Xinjiang Province, has the geological characteristics of epigenetic deposit related to hydrothermal metasomatic process. Mineralization occurs in the Middle Jurassic carbonatite of Longshan Formation and is strictly controlled by the NW trending faults. The main ores are smithsonite and acrusite. The alteration of country rocks are mainly hematitization and ferritization. Sulfur isotopic composition in ore has a wide distribution range (δ34S=-8.49‰~24.88‰), indicating that the S originated from sedimentary strata and the additions of surface fluid. The lead isotopic composition in ore is relatively homogeneous (the values of 206Pb/204Pb, 207Pb/204Pb, 207Pb/204Pb and μ are 18.807-18.822, 15.73-15.756, 39.055-39.168, 9.68-9.73 respectively), with Pb coming from the upper crust. The values ofδ13CV-PDB and δ18OV-SMOW vary from 2.85‰ to 8.25‰, 20.04‰ to 21.07‰ respectively, implying that C and O are from carbonate rocks rather than magmatic hydrothermal fluid. With the analysis of geology of the deposit and isotopic characteristics, Baozishan deposit is regarded as the tectonic hydrothermal-direct metasomatic lead-zinc.
    • HTML全文
  • 加载中
    • 参考文献(41)

  • 陈好寿.铅锌矿床同位素地球化学[M].北京:科学出版社,1997.

    CHEN Haoshou. Isotope Geochemistry of Lead-Zinc Deposits.[M]. Beijing:Science Press,1997.

    杜红星,魏永峰,薛春纪,等. 多宝山铅锌矿床地质特征及地球化学研究[J]. 新疆地质,2012,30(1):52-57.

    DU Hongxing,WEI Yongfeng,XUE Chunji,et al.Geological and Geochemiscal characteristics of Duobaoshan Pb-Zn Deposit in Hetian,Xinjiang[J]. Xinjiang Geology,2012,30(1):52-57.

    董连慧,冯京,刘德权,等.新疆成矿单元划分方案研究[J].新疆地质,2010,28(01):1-15.

    DONG Lianhui, FENG Jing, LIU Dequan, et al. Recearch for Classification of Metallogenic Unit of Xinjiang[J]. Xinjiang Geology,2010,28(01):1-15.

    董连慧,徐兴旺,范廷宾,等. 喀喇昆仑火烧云超大型喷流-沉积成因碳酸盐型Pb-Zn矿的发现及区域成矿学意义[J].新疆地质, 2015, 33(1):41-50.

    DONG Lianhui,XU Xingwang,FAN Tingbin,et al. Discovery of the Huoshaoyun Super-Large Exhalative-SedimentaryCarbonate Pb-Zn Deposit in the Western Kunlun Area and its GreatSignificance for Regional Metallogeny[J]. Xinjiang Geology, 2015, 33(1):41-50.

    高永宝,滕家欣,李侃.喀喇昆仑火烧云超大型铅锌矿床成矿特征与成因[J].矿物学报,2017,(增刊):561-562.

    GAO Yongbao,TENG Jiaxin,LI Kan.Metallogenic characteristics and genesis of HuoshaoyunsuperlargeLead-Zinc deposit in Karakorum[J].Mineralogical Journal,2017,(Suppl.):561-562.

    高峰,菅坤坤,王炬川,等.新疆河尾滩-河西岗地区1:5万矿产地质调查报告[R].西安:陕西省矿产地质调查中心,2019.

    刘家军,何明勤,李志明,等.云南白秧坪银铜多金属矿集区碳氧同位素组成及其意义[J].矿床地质, 2004,23(1):1-10.

    LIU Jiajun, HE Mingqin, LI Zhiming,et al. Oxygen and Carbon Isotopic Geochemistry of BaiyangpingSilver-Copper Polymetallic Ore Concentration Area in LanpingBasin of Yunnan Province and Its Significance[J]. Mineral Deposits, 2004,23(1):1-10.

    刘婷婷,唐菊兴,刘鸿飞,等.西藏墨竹工卡县洞中拉铅锌矿床S、Pb同位素组成及成矿物质来源[J]. 现代地质, 2011, 25(5):869-876.

    LIU Tingting, TANG Juxing, LIU Hongfei,et al. Sulfur and lead isotope composition and tracing for sources of ore-forming materials in the Dongzhongla Pb-Zn deposits in Mozhugongka County,Tibet[J]. Geoscience, 2011, 25(5):869-876.

    李荣社,计文化,杨永成,等.昆仑山及邻区地质[M].北京:地质出版社,2008.

    LI Rongshe,JI Wenhua,YANG Yongcheng,et al.The Geology of Kunlun,China and Adjiacent Areas[M]. Beijing:Geological Publishing House,2008.

    黎敦朋,崔建堂,罗乾周,等. 新疆1:25万岔路口幅(I44C001001)区域地质调查报告[R].西安:陕西省地质调查院,2005.

    陕亮, 郑有业, 许荣科, 等.硫同位素示踪与热液成矿作用研究[J].地质与资源, 2009, 18(3):197-203.

    SHAN Liang,ZHENG Youye,XU Rongke,et al. Review on sulfur isotopic tracing andhydrothermal metallogenesis[J]. Geology and Resources, 2009,18(3):197-203.

    温春齐, 多吉. 矿床研究力法[M].四川:四川科学技术出版社, 2009.

    WEN Chunqi, DUO Ji. Research MethodofDeposit[M]. Sichuan:Sichuan Science and Technology Press, 2009.

    吴开兴,胡瑞忠,毕献武,等.矿石铅同位素示踪成矿物质来源综述[J].地球与环境,2002,30(3):73-81.

    WU Kaixing, HU Ruizhong, BI Xianwu, et al. Ore lead isotopes as a tracer for ore-forming material sources:A review[J]. Earth and Environment, 2002, 30(3):73-81.

    魏永峰,冯邦国,林鑫,等.新疆和田县化石山外围金铅锌矿调查评价报告[R].成都:四川省地质矿产勘查开发局区域地质调查队,2018.

    魏永峰,赵志强,冯邦国,等.新疆和田县化石山一带铅锌矿预查报告[R].成都:四川省地质矿产勘查开发局区域地质调查队,2017.

    杨斌,陈正乐,张青,等.南天山坎岭铅锌矿矿床地质特征及S、Pb同位素特征研究[J].中国地质,2018,45(1):155-167.

    YANG Bin,CHEN Zhengle,ZHANG Qing,et al. Geological characteristics and sulfur and lead isotopes of the Kanlinglead-zincdeposit, Southern Tianshan Mountains[J]. Geology in China,2018, 45(1):155-167.

    张长青, 李厚民, 代军治, 等.铅锌矿床中矿石铅同位素研究[J]. 矿床地质, 25(增刊):213-216.

    ZHANG Changqing, LI Houmin, DAI JunZhi, et al. Lead isotope research onlead-zinc deposits[J]. Mineral Deposits, 2006, 25(suppl.):213-216.

    郑永飞,陈江峰.稳定同位素地球化学[M].北京:科学出版社,2000.

    ZHENG Yongfei, CHEN Jiangfeng. Stable Isotope Geochemistry[M]. Beijing:Science Press,2000.

    赵晓健,伍跃中,王泰山,等. 西昆仑乔尔天山——岔路口地区铅锌矿成矿特征及找矿标志[J].西北地质, 2014, 47(4):245-255.

    ZHAO Xiaojian, WU Yuezhong,WANG Taishan,et al. Metallogenic Characteristics and Prospecting Criteria of Lead-zinc Deposits in Qiao'er Tianshan-Chalukou Region of West Kunlun[J]. Northwestern Geology,2014, 47(4):245-255.

    朱炳泉, 李献华. 地球科学中同位素体系理论与应用-兼论中国大陆壳幔演化[M]. 北京:科学出版社,1998.

    ZHU Bingquan, LI Xianhua. The Theory and Application of Isotopic System in Earth Science-Crust Mantle Evolution in China[M]. Beijing:Science Press, 1998.

    CLAYPOOL GE, HOLSER WT, KAPLAN IR, et al. The age curves of sul fur and oxygen isotopes in marine sulfate and their mutual interpretation[J].Chemical Geology,1980, 28:199-260.

    OHMOTOH.Stable isotope geochemistry of ore deposits[J]. Reviews in Mineralogy,1986,16(1):491-559.

    OHMOTO H,GOLDHABER M B.Sulfur and carbon isotopes[J].Geochemistry of Hydrothermal Ore Deposits,1997,3:517-611.

    ZARTMANRE, DOEBR. Plumbotectonics-the model[J]. Tectonopysics,1981,75(1-2):135-162.

    TAYLOR BE. Stable isotope geochemistry of ore-forming fluids[J]. Mineralogist Association of Canada:Short Course Handbook, 1987a,13:337-445.

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  921
  • PDF下载数:  560
  • 施引文献:  0
出版历程
收稿日期:  2019-03-09
修回日期:  2019-10-30

目录

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