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青藏高原铅锌矿资源特征
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  • 英文篇名:Geological characteristics of lead-zinc ore deposits in Qinghai-Tibet Plateau
  • 作者:王立强 ; 唐菊兴 ; 旦真王修 ; 王勇 ; 李壮
  • 英文作者:WANG Liqiang;TANG Juxing;DANZHEN Wangxiu;WANG Yong;LI Zhuang;Institute of Mineral Resources, Chinese Academy of Geological Sciences;School of Earth and Resources, China University of Geosciences;
  • 关键词:铅锌矿 ; 开发利用前景 ; 青藏高原
  • 英文关键词:lead-zinc mineral resource;;exploration and utilization;;Qinghai-Tibet Plaetu
  • 中文刊名:KJDB
  • 英文刊名:Science & Technology Review
  • 机构:中国地质科学院矿产资源研究所;中国地质大学(北京)地球科学与资源学院;
  • 出版日期:2017-06-28
  • 出版单位:科技导报
  • 年:2017
  • 期:v.35;No.522
  • 基金:国家自然科学基金项目(41403040);; 国土资源部公益性行业科研专项(201511017,201511022-02)
  • 语种:中文;
  • 页:KJDB201712020
  • 页数:6
  • CN:12
  • ISSN:11-1421/N
  • 分类号:85-90
摘要
铅锌矿为青藏高原十分重要的优势矿种,尤其西藏冈底斯地区已经成为中国铅锌多金属矿产资源接续基地。本文总结了青藏高原铅锌矿分布情况、形成时代、成因类型、资源储量等特征,剖析了其开发利用前景与民生经济发展之关系。
        The Pb-Zn mineral resource is one of the very important mineral resources in the Qinghai-Tibet Plateau, especially, in the Gangdese region of Tibet, which becomes the substitutable base of Pb-Zn polymetallic mineral resources in China. Based on previous studies, the distribution, the mineralization ages, the deposit type and the resource reserves of the Pb-Zn ore deposits in the Qinghai-Tibet Plateau are reviewed in this paper. And then, the relationship between the utilization prospects of the mineral resources and the economic development is analyzed.
引文
[1]宋玉财,侯增谦,杨天南,等.“三江”喜马拉雅期沉积岩容矿贱金属矿床基本特征与成因类型[J].岩石矿物学杂志,2011,30(3):355-380.Song Yucai,Hou Zengqian,Yang Tiannan,et al.Sediment-hosted Hi-malayan base metal deposits in Sanjiang region:characteristics and ge-netic types[J].Acta Petrologica et Minerlogica,2011,30(3):355-380.
    [2]潘桂棠,莫宣学,侯增谦,等.冈底斯造山带的时空结构及演化[J].岩石学报,2006,22(3):521-533.Pan Guitang,Mo Xuanxue,Hou Zengqian,et al.Spatial-temporal frame-work of the Gangdese Orogenic belt and its evolution[J].Acta Petrologi-ca Sinica,2006,22(3):521-533.
    [3]丛源,董庆吉,肖克炎.三江成矿带斑岩型矿床成矿模式与找矿方向研究[J].地质学刊,2013,37(4):562-569.Cong Yuan,Dong Qingji,Xiao Keyan.Study on metallogenic model andore exploration of porphyry deposits in Sanjiang metallogenic belt[J].Journal of Geology,2013,37(4):562-569.
    [4]高兰,肖克炎,丛源,等.西南三江锌铅银铜锑金成矿带成矿特征及资源潜力[J].地质学报,2016,90(7):1650-1667.Gao Lan,Xiao Keyan,Cong Yuan,et al.Metallogenic characteristicsand mineral resource potential of the southwestern Sanjiang Zn-Pb-Cu-Ag-Sb-Au metallogenic belt[J].Acta Geologica Sinica,2016,90(7):1650-1667.
    [5]王立强.印度-亚洲大陆碰撞早期成矿聚集带——念青唐古拉铅锌多金属成矿作用研究[D].北京:中国地质大学,2016.Wang Liqiang.Metallogenic accumulation during the early stage of In-dia-Asia continental collision:Study on the Pb-Zn polymetallic miner-alization in Nyainqentanglha area[D].Beijing:China University of Geo-sciences,2016.
    [6]王学求,申伍军,张必敏,等.地球化学块体与大型矿集区的关系——以东天山为例[J].地学前缘,2007,14(5):116-123.Wang Xueqiu,Shen Wujun,Zhang Bimin,et al.Relationship of geo-chemical blocks and ore districts:Examples from Eastern Tianshanmetallogenic belt:Xinjiang,China[J].Earth Science Frontiers,2007,14(5):116-123.
    [7]刘长征,陈岳龙,许光,等.地球化学块体理论在青海沱沱河地区铅锌资源潜力预测中的应用[J].地学前缘,2011,18(5):271-282.Liu Changzheng,Chen Yuelong,Xu Guang,et al.The application ofgeochemical block theory to lead and zinc resource assessment in Tuo-tuohe area of Qinghai Province[J].Earth Science Frontiers,2011,18(5):271-282.
    [8]李玉龙,杨竹森,田世洪,等.“三江”中段两类碳酸盐岩容矿铅锌矿化成因的相关性——来自稀土元素地球化学研究的启示[J].岩石矿物学杂志,2015,34(5):648-664.Li Yulong,Yang Zhusen,Tian Shihong,et al.Genetic relationship be-tween the two types of carbonate-hosted Pb-Zn deposits in the middlepart of the'Sanjiang'metallogenic belt:Information from REE study[J].Acta Petrologica et Mineralogica,34(5):648-664.
    [9]高一鸣,陈毓川,唐菊兴,等.西藏工布江达地区亚贵拉铅锌钼矿床Re-Os测年及其地质意义[J].地质通报,2011,30(7):1027-1036.Gao Yiming,Chen Yuchuan,Tang Juxing,et al.Re-Os dating of molyb-denite from the Yaguila porphyry molybdenum deposit in Gongbogyam-da area,Tibet,and its geological significance[J].Geological Bulletin ofChina,2011,30(7):1027-1036.
    [10]费光春,温春齐,周雄,等.西藏洞中拉铅锌矿床石英激光探针40Ar-39Ar定年及地质意义[J].矿物岩石,2010,30(3):38-43.Fei Guangchun,Wen Chunqi,Zhou Xiong,et al.Laser micro-probe40Ar-39Ar geochronology of quartz from Dongzhongla lead-zincdeposit in Tibet and its significance[J].Journal of Mineralogy and Pe-trology,2010,30(3):38-43.
    [11]辛存林,都卫东,张育平,等.西藏洞中松多铅锌多金属矿床地质特征及成因[J].兰州大学学报(自然科学版),2013,49(1):24-31.Xin Cunlin,Du Weidong,Zhang Yuping,et al.A preliminary study ofthe geologic characteristics and genesis of the Dongzhongsongduo lead-zinc polymetallic deposit,Tibet[J].Journal of Lanzhou University(Natural Sciences),2013,49(1):24-31.
    [12]Wang L Q,Tang J X,Deng J,et al.The Longmala and Mengya'askarn Pb-Zn deposits,Gangdese region,Tibet:Evidence from U-Pband Re-Os geochronology for formation during early India-Asia colli-sion[J].International Geology Review,2015,57(14):1825-1842.
    [13]王立强,唐菊兴,郑文宝,等.西藏玛雄郎铅锌矿区那舵松多矿段黑云母40Ar-39Ar年代学及硫-铅同位素地球化学[J].大地构造与成矿学,2014,38(4):954-961.Wang Liqiang,Tang Juxing,Zheng Wenbao,et al.40Ar-39Ar dating,sulfur and lead isotope geochemistry of the Narusongduo Ore sectionof Maxionglang Pb-Zn ore deposit,Tibet[J].Geotectonica et Metalloge-nia,2014,38(4):954-961.
    [14]Li X F,Wang C Z,Mao W,et al.The fault-controlled skarn W-Mopolymetallic mineralization during the main India-Eurasia collision:Example from Hahaigang deposit of Gangdese metallogenic belt of Ti-bet[J].Ore Geology Reviews,2014,58:27-40.
    [15]Wang L Q,Cheng W B,Tang J X,et al.U-Pb geochronology,geo-chemistry,and H-O-S-Pb isotopic compositions of the Leqingla andXin'gaguo skarn Pb-Zn polymetallic deposits,Tibet,China[J].Journalof Asian Earth Sciences,115:80-96.
    [16]纪现华,杨竹森,于玉帅,等.西藏纳如松多铅锌矿床岩体形成机制:岩浆锆石证据[J].矿床地质,2012,31(4):758-774.Ji Xianhua,Yang Zhusen,Yu Yushuai,et al.Formation mechanism ofmagmatic rocks in Narusongduo lead-zinc deposit of Tibet:Evidencefrom magmatic zircon[J].Mineral Deposits,2012,31(4):758-774.
    [17]纪现华,孟祥金,杨竹森,等.西藏纳如松多引爆角砾岩型铅锌矿床绢云母Ar-Ar定年及其地质意义[J].地质与勘探,2014,50(2):281-290.Ji Xianhua,Meng Xiangjin,Yang Zhusen,et al.The Ar-Ar geochro-nology of sericite from the cryptoexplosive breccia type Pb-Zn depositin Narusongdu,Tibet and its geological significance[J].Geology andExploration,2014,50(2):281-290.
    [18]魏启荣,刘小念,丁鹏飞,等.冈底斯中段扎扎龙矿区闪长岩体锆石U-Pb年代学-岩石地球化学特征及其意义[J].吉林大学学报(地球科学版),2015,45(5):1405-1417.Wei Qirong,Liu Xiaonian,Ding Pengfei,et al.Zircon U-Pb Chronolo-gy,Geochemical Characteristics and Significance of diorites in miningarea of Zhazhalong in mid-gangdese[J].Journal of Jilin University(Earth Science Edition),2015,45(5):1405-1417.
    [19]高顺宝,郑有业,田立明,等.西藏查个勒铜铅锌矿成岩成矿时代及意义[J].地球科学,2012,37(3):507-514.Gao Shunbao,Zheng Youye,Tian Liming,et al.Geochronology of mag-matic Intrusions and mineralization of Chagele copper-lead-zinc de-posit in Tibet and its implications[J].Earth Science,2012,37(3):507-514.
    [20]段志明,李光明,李应栩,等.中冈底斯成矿段龙根铅锌矿床含矿斑岩年代学与地球化学特征[J].矿床地质,2014,33(3):625-638.Duan Zhiming,Li Guangming,Li Yingxu,et al.Geochronology andgeochemical charateristics of ore-bearing porphyry in Longgen lead-zinc deposit of middle-Gangdese metallogenic betl,Tibet[J].MineralDeposits,2014,33(3):625-638.
    [21]赵晓燕,杨竹森,刘英超,等.西藏夏垅铅锌银矿床绢云母40Ar/39Ar年龄及其地质意义[J].矿床地质,2013,32(5):963-971.Zhao Xiaoyan,Yang Zhusen,Liu Yingchao,et al.40Ar-39Ar dating ofsericite from Xialong Pb-Zn-Ag deposit and its geological significance[J].Mineral Deposits,2013,32(5):963-971.
    [22]应立娟,王登红,唐菊兴,等.西藏甲玛铜多金属矿辉钼矿Re-Os定年及其成矿意义[J].地质学报,2010,84(8):1165-1174.Ying Lijuan,Wang Denghong,Tang Juxing,et al.Re-Os dating of mo-lybdenite from the Jiama copper polymetallic deposit in Tibet and itsmetallogenic significance[J].Acta Geologica Sinica,2010,84(8):1165-1174.
    [23]Wang L Q,Chen Y C,Tang J X,et al.LA-ICP-MS zircon U-Pb dat-ing of intermediate-acidic intrusive rocks and molybdenite Re-Os dat-ing from the Bangpu Mo(Cu)deposit,Tibet and its geological implica-tion[J].Acta Geologica Sinica,2012,86(5):1225-1240.
    [24]李光明,芮宗瑶,王高明,等.西藏冈底斯成矿带甲玛和知不拉铜多金属矿床的Re-Os同位素年龄及其意义[J].矿床地质,2005,24(5):481-489.Li Guangming,Rui Zongyao,Wang Gaoming,et al.Molybdenite Re-Os dating of Jiama and Zhibula polymetallic copper deposits in Gang-dese metallogenic belt of Tibet and its significance[J].Mineral Depos-its,2005,24(5):481-489.
    [25]田世洪,杨竹森,侯增谦,等.玉树地区东莫扎抓和莫海拉亨铅锌矿床Rb-Sr和Sm-Nd等时线年龄及其地质意义[J].矿床地质,2009,28(6):747-758.Tian Shihong,Yang Zhusen,Hou Zengqian,et al.Rb-Sr and Sm-Ndisochron ages of Dongmozhazhua and Mohailaheng Pb-Zn ore depos-its in Yushu area,southern Qinghai and their geological implications[J].Mineral Deposits,2009,28(6):747-758.
    [26]Liu Y C,Hou Z Q,Yang Z S,et al.Geology and chronology of theZhao fayong carbonate-hosted Pb-Zn ore cluster:Implication for re-gional Pb-Zn metallogenesis in the Sanjiang belt,Tibet[J].GondwanaResearch,2016,35:15-26.
    [27]唐菊兴,丁帅,孟展,等.西藏林子宗群火山岩中首次发现低硫化型浅成低温热液型矿床——以斯弄多银多金属矿为例[J].地球学报,2016,37(4):461-470.Tang Juxing,Ding Shuai,Meng Zhan,et al.The first discovery of thelow sulfidation epithermal deposit in Linzizong volcanics,Tibet:Acase study of the Sinongduo Ag polymetallic deposit[J].Acta Geoscien-tica Sinica,2016,37(4):461-470.
    [28]刘英超,纪现华,侯增谦,等.一个与岩浆作用有关的独立铅锌成矿系统的建立——以西藏纳如松多铅锌矿床为例[J].岩石矿物学杂志,2015,34(4):539-556.Liu Yingchao,Ji Xianhua,Hou Zengqian,et al.The establishment ofan independent Pb-Zn mineralization system related to magmatism:acase study of the Narusongduo Pb-Zn deposit in Tibet[J].Acta Petro-logica et Mineralogica,2015,34(4):539-556.
    [29]刘英超.青藏高原三江中段碳酸盐岩容矿铅锌矿床成矿特征与成因研究[D].北京:中国地质科学院,2012.Liu Yingchao.Characteristics and metallogenic genesis of the carbon-ate-hosted lea-zinc deposits in the middle part of Sanjiang area,Ti-betan plateau[D].Beijing:Chinese Academy of Geological Sciences,2012.
    [30]宋玉财,侯增谦,王贵仁,等.“三江”北段沱沱河地区的成矿规律与找矿方向[J].矿床地质,2015,34(1):1-20.Song Yucai,Hou Zengqian,Wang Guiren,et al.Metallogenic regulari-ty and ore exploration targeting in Tuotuohe area,northern Sanjiangorogenic belt[J].Mineral Deposits,2015,34(1):1-20.
    [31]段志明,李光明,王保弟,等.西藏中冈底斯成矿带查个勒铅锌矿床含矿斑岩年代学及其地质意义[J].吉林大学学报(地球科学版),2015,45(6):1667-1690.Duan Zhiming,Li Guangming,Wang Baodi,et al.Geochronology andits geological significance of the ore-bearing porphyry in Chagelelead-zinc deposit in middle-Gangdese metallogenic belt,Tibet[J].Earth Science,2015,45(6):1667-1690.
    [32]罗生福.青海多才玛铅锌资源量达600万吨[N].中国国土资源报,2014-11-11.Luo Shengfu.Lead-Zinc resource of the Duocaima Pb-Zn depositamounting to 600 million tons[N].China Land and Resource News,2014-11-11.

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