吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 722-735.doi: 10.13278/j.cnki.jjuese.201603110

• 地质与资源 • 上一篇    下一篇

滇东北Pb-Zn-(Ag)多金属矿床找矿突破关键基础地质问题

唐忠1, 李文昌2, 王长兵3, 明添学1, 李蓉1, 包从法4, 王珏2, 李永平1   

  1. 1. 云南省地质调查院, 昆明 650051;
    2. 云南省地质调查局, 昆明 650051;
    3. 云南省核工业209地质大队, 昆明 650032;
    4. 云南省国土资源规划设计研究院, 昆明 650051
  • 收稿日期:2015-10-15 出版日期:2016-05-26 发布日期:2016-05-26
  • 作者简介:唐忠(1985),男,工程师,主要从事矿产勘查与评价、找矿预测方面的研究工作,E-mail:99688182@qq.com
  • 基金资助:

    云南省科技创新人才计划（2013HA001）；国家重点基础研究发展计划（国家“973”计划）项目（2015CB452605）

Critical Geological Issues About Ore-Prospecting Breakthrough of Pb-Zn-(Ag) Polymetallic Deposit in Northeast Yunnan

Tang Zhong1, Li Wenchang2, Wang Changbing3, Ming Tianxue1, Li Rong1, Bao Congfa4, Wang Jue2, Li Yongping1   

  1. 1. Institute of Yunnan Geology Survey, Kunming 650051, China;
    2. Bureau of Yunnan Geology Survey, Kunming 650051, China;
    3. Team 209 of Yunnan Nuclear Industry, Kunming 650032, China;
    4. Mineral and Land Resources Institute of Yunnan, Kunming 650051, China
  • Received:2015-10-15 Online:2016-05-26 Published:2016-05-26
  • Supported by:

    Supported by the Plan of Science and Technology Innovative Talents in Yunnan Province(2013HA001) and National Program on Key Basic Research Project (2015CB452605)

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摘要：

梳理过去几十年对滇东北地区铅锌（银）多金属矿的科学研究成果和找矿勘查经验发现，一些影响找矿突破的关键基础地质问题始终难以达成共识或长久未被解决。文章以“三位一体”找矿预测方法为指导，围绕成矿地质体、成矿构造及成矿作用特征标志等直接影响推测矿体（床）全部地质特征的内容进行系统论述，综合分析认为：滇东北地区主要产出以茂租铅锌矿为代表的层控型矿床和以乐红铅锌矿为代表的构造控矿型矿床，成矿地质体为高原陆核地体系统内的坳陷盆地，成矿构造主要为SN向深断裂带、NW向深断裂带及NE向深断裂所引起的次生构造，矿床成因与沉积及后期热液改造有直接关系，成矿时代主要集中在晚三叠世，成矿物质主要来源于震旦系碳酸盐岩地层，成矿机制为古特提斯向扬子板块西南缘俯冲驱动陆内盆地的热、气、液反复循环，不断改造-萃取-富集成矿。

关键词: 铅锌(银)多金属矿床, 关键基础地质, 三位一体, 滇东北

Abstract:

Studies of the past few decades of research data and exploration experience about Pb-Zn-(Ag) polymetallic deposit in northeast Yunnan indicate that there are several critical geological issues about prospecting breakthrough difficult to be understood and resolved. According to the "Geological Body-Structure-Mineralization" prospecting prediction method, the metallogenic geological body, ore-forming structure and mineralization characteristic indications can directly influence all geological features of the deposit. However, combined with previous opinions and the latest information, we proposed that there are two main kinds of Pb-Zn deposit discovered in the area, strata-bound and structure-controlling deposits. The metallogenic geological body was depression basin of plateau land system, and main ore-controlling structure were some secondary fractures caused by SN-NW-NE trending deep fault zone. It is considered that the genesis of deposit is closely related to sedimentary and epigenetic hydrothermal transformation, the mineralization ages of these deposits are mainly in the Late Triassic, the metallogenic material mainly originated from carbonate formation of Sinian System, and their metallogenetic mechanism can be concluded as followings, the subduction of the Paleo-Tethys ocean to the southwestern edge of the Yangtze plate caused the recycling action of hot, gas and hydrothermal fluid in intracontinental basin, which resulted in consist transforming, extraction and enrichment of metallogenic elements, and led to the polymetallic mineralization.

Key words: Pb-Zn-(Ag) polymetallic deposit, critical geology, geological body-structure-mineralization, northeast Yunnan

中图分类号: 

  • P618.4

[1] 叶天竺.矿床模型综合地质信息预测技术方法理论框架[J].吉林大学学报(地球科学版),2013,43(4):1053-1072. Ye Tianzhu. Theoretical Framework of Methodology of Deposit Modeling and Integrated Geological Information for Mineral Resource Potential Assessment[J]. Journal of Jilin University(Earth Science Edition), 2013,43(4):1053-1072.

[2] 叶天竺,吕志成,庞振山,等.勘查区找矿预测理论与方法[M].北京:地质出版社,2014:1-700. Ye Tianzhu,Lü Zhicheng,Peng Zhenshan,et al. Metallogenic Prognosis Theories and Methods in Exploration Areas[M]. Beijing:Geologyical Publishing House,2014:1-700.

[3] 谭清立,高建国,刘心开.川滇黔接壤区铅锌矿分布规律[J].河南科学,2013,31(9):1470-1475. Tan Qingli,Gao Jianguo,Liu Xinkai. Distribution Regularity of the Sichuan-Yunnan-Guizhou Pb-Zn Metallogenic Area[J]. Henan Science,2013,31(9):1470-1475.

[4] 陈大,吴林峰.川滇黔相邻区铅锌矿床分布特征及成矿规律[J].四川地质学报,2012,32(3):304-308. Chen Da,Wu Linfeng. Distribution and Metallogeny of Pb-Zn Deposits in the Sichuan-Yunnan-Guizhou Border Region[J]. Geology Edition of Sichuan, 2012, 32(3):304-308.

[5] 韩润生,刘丛强,黄智龙,等.论云南会泽富铅锌矿床成矿模式[J].矿物学报,2001,21(4):674-680. Han Runsheng,Liu Congqiang,Huang Zhilong,et al. Genesis Modeling of Huize Lead-Zinc Ore Deposit in Yunnan[J]. Acta Mineralogica Sinica,2001,21(4):674-680.

[6] 韩润生,刘丛强,黄智龙,等.云南会泽铅锌矿床构造控矿及断裂构造岩稀土元素组成特征[J].矿物岩石,2001,20(4):11-18. Han Runsheng,Liu Congqiang,Huang Zhilong,et al. Characteristics of Ore-Controlling Structures and REE Composition of Fault Rocks in Huize Lead-Zinc Deposit,Yunnan[J]. Journal Mineral Petrol,2001,20(4):11-18.

[7] 韩润生,陈进,黄智龙,等.构造成矿动力学及隐伏矿定位预测:以云南会泽铅锌(银、锗)矿床为例[M].北京:科学出版社,2006:1-239. Han Runsheng,Chen jin,Huang Zhilong,et al. Dynamics of Tectonic Ore-Forming Processes and Localization-Prognosis of Concealed Orebodies-As Exemplified by the Super-Large Zn-Pb-(Ag-Ge) District,Yunnan[M]. Beijing:Science Press,2006:1-239.

[8] 芮宗瑶, 叶锦华, 张立生, 等.扬子克拉通周边及其隆起边缘的铅锌矿床[J].中国地质, 2004, 31(4):337-346. Rui Zongyao,Ye Jinhua,Zhang Lisheng,et al. Pb-Zn Depsits on the Perimeter of the Yangtze Craton and on the Margins of Its Uplifts[J]. China in Geology,2004,31(4):337-346.

[9] 黄智龙,陈进,刘丛强,等. 峨眉山玄武岩与铅锌矿床成矿关系初探:以云南会泽铅锌矿床为例[J].矿物学报,2001,21(4):681-688. Huang Zhilong,Chen Jin,Liu Congqiang,et al. Preliminary Discussion on the Genetic Relationship Between Emeishan Basalts and Pb-Zn Deposits as Exemplified by the Huize Pb-Zn Deposit,Yunnan Province[J]. Acta Mineralogica Sinica, 2001,21(4):681-688.

[10] 鲍淼,周家喜,黄智龙,等.铅锌矿床定年方法及川-滇-黔铅锌成矿域年代学研究进展[J].矿物学报,2011,31(3):391-396. Bao Miao,Zhou Jiaxi,Huang Zhilong,et al. Dating Methods for Pb-Zn Deposits and Chronology Research Progress of Sichuan-Yunnan-Guizhou Pb-Zn Metallo-genic Province:A Review[J]. Acta Mineralogica Sinica,2011,31(3):391-396.

[11] 王奖臻,李朝阳,李泽琴,等.川滇黔交界地区密西西比河谷型铅锌矿床与美国同类矿床的对比[J].矿物岩石地球化学通报,2002,21(2):127-132. Wang Jiangzhen,Li Chaoyang,Li Zeqin,et al. The Comparison of Mississippi Valley-Type Lead-Zinc Deposits in Southwest of China and in Mid-Continent of United States[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2002,21(2):127-132.

[12] 张长青,毛景文,吴锁平,等.川滇黔地区MVT铅锌矿床分布、特征及成因[J].矿床地质,2005,24(3):336-348. Zhang Changqing,Mao Jingwen,Wu Suoping,et al. Distribution,Characteristics and Genesis of Mississippi Valley-Type Lead-Zinc Deposits in Sichuan-Yunnan-Guizhou Area[J]. Mineral Deposits,2005,24(3):336-348.

[13] 李文博,黄智龙,陈进,等. 云南会泽超大型铅锌矿床成矿物质来源:来自矿区外围地层及玄武岩成矿元素含量的证据[J]. 矿床地质,2002,21(增刊):413-416. Li Wenbo,Huang Zhilong,Chen Jin,et al. Sources of Ore-Forming Materials in Huize Superlarge Zinc-Lead Deposit,Yunnan Province:Evidence from Contents of Ore-Forming Element in Strata and Basalts from Margin of Ore District[J]. Mineral Deposit,2002,21(Sup.):413-416.

[14] 韩润生,胡煜昭,王学琨,等.滇东北富锗银铅锌多金属矿集区矿床模型[J].地质学报,2012,86(2):280-294. Han Runsheng,Hu Yuzhao,Wang Xuekun,et al. Mineralization Model of Rich Ge-Ag-Bearing Zn-Pb Polymetallic Deposit Concentrated District in Northeastern Yunnan,China[J]. Acta Mineralogica Sinica,2012,86(2):280-294.

[15] Leach D L,Bradley D C,Huston D,et al. Sediment-Hosted Lead-Zinc Deposits in Earth History[J]. Econ Geol,2010,105:593-625.

[16] 张长青.中国川滇黔交界地区密西西比型(MVT)铅锌矿床成矿模型[D].北京:中国地质科学院,2008. Zhang Changqing. The Genetic Model of Mississippi Valley-Type Deposits in the Boundary Area of Sichuan,Yunnan and Guizhou Provinces,China[D]. Beijing:Chine Academy of Geological Sciences,2008.

[17] 柳贺昌,林文达.滇东北铅锌银矿床规律研究[M].昆明:云南大学出版社,1999:1-468. Liu Hechang,Lin Wenda. Study on Pb-Zn-Agore Deposits Law in Northeast Yunnan Province[M].Kunming:Yunnan University Press,1999:1-468.

[18] 王宝禄,李丽辉,李本茂,等.近20年云南勘察地球物理(化学)回顾与展望[J].云南大学学报(自然科学版),2007, 29(增刊1):542-547. Wang Baolu,Li Lihui,Li Benmao,et al. The Retrospect and Prospect of Earthly Physics(Chemistry) During the Last 20 Years in Yunnan Province[J]. Journal of Yunnan University(Natural Sciences Edition),2007,29(Sup.1):542-547.

[19] 李丽辉,陈明伟,王宝禄.近10年来云南省物化探工作进展与主要成果[J]. 云南大学学报(自然科学版),2012,34(增刊2):125-133. Li Lihui,Chen Mingwei,Wang Baolu. The Progress and Results of Geophysical and Geochemistry Prospecting During the Last 10 Years in Yunnan Province[J]. Journal of Yunnan University(Natural Sciences Edition),2012,34(Sup.2):125-133.

[20] 王雅丽,崔银亮.滇东北北部遥感蚀变信息提取与研究意义[J].云南地质,2012,31(4):485-488. Wang Yali,Cui Yinliang. The Significance of Abstract Ion and Study of Remote-Sensing Alteration Information of N Part in NE Yunnan[J]. Geology Yunnan,2012,31(4):485-488.

[21] 周云满.物探方法在滇东北地区寻找隐伏矿床的应用效果[J].地质与勘探,2006,42(3):81-85. Zhou Yunman. Application Effects of Geophysical Prospecting Method for Hidden Deposits in the Northeastern Yunnan[J]. Geology and Prospecting,2006,42(3):81-85.

[22] 张云峰,李领军,张蓉.遥感构造解译在滇东北地区成矿预测中的半定量应用[J].矿产与地质,2007,21(3):358-362. Zhang Yunfeng,Li Lingjun,Zhang Rong. Semiquan-titative Application of Remote Sensing Structure Explanation to Ore Prediction in Northeast Yunnan Area[J]. Mineral Resources and Geology, 2007,21(3):358-362.

[23] 王雅丽,崔银亮. 滇东北及毛坪铅锌矿遥感地质与成矿预测[J].云南地质,2010,29(4):438-443. Wang Yali,Cui Yinliang. The Remote Sensing Geological Characteristics and Metallogenesis Prognosis of Maoping Pb-Zn Deposit in NE Yunnan[J].Geology Yunnan,, 2010,29(4):438-443.

[24] 李波,韩润生,顾晓春,等.云南巧家松梁矿床Ⅰ号矿体构造原生晕轴向分带序列[J].矿产与地质,2009,23(2):97-103. Li Bo,Han Runsheng,Gu Xiaochun,et al. Axial Zonality Sequence of Tectonic Primary Halos of No.1 Orebody in the Songliang Lead-Zinc Deposit,Qiaojia of Yunnan Province[J]. Mineral Resources and Geology, 2009, 23(2):97-103.

[25] 丁德生.乐红铅锌矿床综合找矿模型的建立及重要性[J]. 有色金属设计,2007,34(2):11-20. Ding Desheng. Establishment of Ore-Prospecting Model for Yunnan Lehong Pb-Zn Deposit and the Significance[J].Nonferrous Metals Design,2007,34(2):11-20.

[26] 周云满.滇东北乐红铅锌矿床地质特征及找矿远景[J].地质地球化学,2003,31(4):17-22. Zhou Yunman. Geological Characteristics of the Lehong Lead-Zinc Deposit in Northeastern Yunnan and Its Ore-Search Prospects[J]. Geology-Geochemistry,2003,31(4):17-22.

[27] 高航校,任小华,郭健,等. 茂租铅锌矿地质-地球物理特征及矿体预测研究[J].矿产与地质,2011,25(2):152-157. Gao Hangxiao,Ren Xiaohua,Guo Jian,et al. Geological-Gephysical Characteristics and Orebody Prediction of Maozu Lead-Zinc Deposit[J]. Mineral Resources and Geology,2011,25(2):152-157.

[28] 刘文周.云南茂租铅锌矿矿床地质地球化学特征及成矿机制分析[J].成都理工大学学报,2009,36(5):480-488. Liu Wenzhou. Geological and Geochemical Charac-teristics and Metallogenic Mechanism Analysis of the Pb-Zn Deposit in Maozu,Yunnan,China[J]. Journal of Chengdu University of Technology,2009,36(5):480-488.

[29] 周云满.乐马厂银矿逆冲推覆构造特征及控矿作用[J].矿床地质,2001,20(3):271-278. Zhou Yunman. Characteristics and Ore-Controlling Role of the Thrusting Nappe Structure in the Lemachang Silver Deposit[J]. Mineral Deposits,2001,20(3):271-278.

[30] 张志斌,李朝阳,涂光炽,等.川滇黔接壤区铅锌矿床产出的大地构造演化背景及成矿作用[J].大地构造与成矿学,2006, 30(3):343-354. Zhang Zhibin,Li Zhaoyang,Tu Guangchi,et al. Geotectonic Evolution Background and Ore-Forming Process of Pb-Zn Deposits in Chuan-Dian-Qian Area of Southwest China[J].Geotectonica et Metallogenia,2006,30(3):343-354.

[31] 任治机,朱智华,赵重顺.云南地体构造与成矿作用[M].北京:冶金工业出版社,1996:1-185. Ren Zhiji,Zhu Zhihua,Zhao Chongshun. Terrane Tectonics and Metallogensis in Yunnan,China[M]. Beijing:Metallurgical Industry Press,1996:1-185.

[32] 吴越.川滇黔地区MVT铅锌矿床大规模成矿作用的时代与机制[D].北京:中国地质大学,2013. Wu Yue. The Age and Ore-Forming Process of MVT Deposits in the Boundary Area of Sichuan-Yunnan-Guizhou Provinces,Southwest China[D]. Beijing:China University of Geosciences,2013.

[33] 张长青,叶天竺,吴越,等.Si/Ca界面对铅锌矿床定位的控制作用及其找矿意义[J].矿床地质,2012,31(3):405-416. Zhang Changqing,Ye Tianzhu,Wu Yue,et al. Discussion on Controlling Role of Si-Ca Boundary in Locating Pb-Zn Deposits and Its Prospecting Signi-ficance[J]. Mineral Deposits,2012,31(3):405-416.

[34] 刘英俊,曹励明,李兆麟,等.元素地球化学[M]. 北京:科学出版社,1984:1-480. Liu Yingjun,Cao Liming,Li Zhaolin,et al. Element Geochemistry[M]. Beijing:Science Press,1984:1-480.

[35] 王乾,安匀玲,顾雪祥,等. 康滇地轴东缘典型铅锌矿床半生分散元素镉锗镓赋存状态与富集规律研究[J]. 地球与环境,2010,38(3):286-294. Wang Qian,An Yunling,Gu Xuexiang,et al. The Research of Occurrence State and Enrichment Law of Associated Dispersed Elements Gd,Ge,and Ga of Typical Lead-Zinc Deposits in the Eastern Edge of Kangdian Axis,China[J]. Earth and Environment,2010,38(3):286-294.

[36] 付绍洪,顾雪祥,王乾,等. 扬子地块西南缘铅锌矿床Cd、Ge与Ga富集规律初步研究[J]. 矿物岩石地球化学通报,2004,23(2):105-108. Fu Shaohong,Gu Xuexiang,Wang Qian,et al. A Preliminary Study on the Enrichment Regularity of Dispersed Elements Cd,Ge and Ga in Lead-Zinc Deposits in the SW Margin of the Yangtze Platform[J]. Bulletin of Mineralogy Petrology and Geochemistry,2004,23(2):105-108.

[37] 薛步高.超大型会泽富锗铅锌矿复合成因[J].云南地质,2006,25(2):143-159. Xue Bugao. The Composite Genesis of Huize Super-Large Pb-Zn Deposit Rich in Ge[J]. Yunnan Geology, 2006,25(2):143-159.

[38] 涂光炽.从一个侧面看矿床事业的发展:若干重要矿床领域的新进展及找矿思维的开拓[J]. 矿床地质,2002,21(2):97-105. Tu Guangchi. Glimpse of Past Achievements in Ore Exploration and Research Work[J]. Mineral Deposits,2002,21(2):97-105.

[39] 周朝宪.滇东北麟麒厂锌铅矿床成矿金属来源、成矿流体特征和成矿机理研究[D].贵阳:中国科学院地球化学研究所, 1996. Zhou Chaoxian. The Origin of the Mineralizing Metals, the Geochemical Characteristics of Ore-Forming Fluid,and the Genesis of Qilinchang Zn-Pb Deposits,Northeast Yunnan Province,China[D]. Guiyang:Institute of Geochemistry,Chinese Academy of Sciences,1996.

[40] 邵世才,李朝阳.扬子地块西缘震旦系灯影组层控铅锌矿床的成矿规律及形成超大型矿床的可能性[J].云南地质,1996,15(4):345-350. Shao Shicai,Li Zhaoyang. Metallogenetic Rules of the Stratabound Pb-Zn Deposit in Dengying Formation of the West Margin of Yangzi Massif and Its Possibility of Forming Super-Large Ore Deposit[J].Yunnan Geology,1996,15(4):345-350.

[41] 张振亮,黄智龙,饶冰,等.会泽铅锌矿床的成矿流体来源:来自水-岩反应的证据[J]. 吉林大学学报(地球科学版),2005,35(5):587-592. Zhang Zhenliang,Huang Zhilong,Rao Bing,et al. The Sources of Ore-Forming Fluid in the Huize Lead-Zinc Ore Deposits:Evidences for Water-Rock Reaction[J]. Journal of Jilin University(Earth Science Edition),2005,35(5):587-592.

[42] 张云湘,骆耀南,杨崇喜,等.攀西裂谷[M].北京:地质出版社,1988:1-320 Zhang Yunxiang,Luo Yaonan,Yang Congxi,et al. Panxi Rift[M]. Beijing:Geologyical Publishing House,1988:1-320.

[43] 王奖臻,李朝阳,李泽琴,等.川滇地区密西西比河谷型铅锌矿床成矿地质背景及成因探讨[J].地质地球化学,2001,29(2):41-45. Wang Jianhzhen,Li Zhaoyang,Li Zeqin,et al. The Geological Setting,Characters and Origin of Mississippi Valley-Type Pb-Zn Deposits in Sichuan and Yunnan Province[J]. Geology-Geochemistry,2001,29(2):41-45.

[44] 张长青,毛景文,刘峰,等.云南会泽铅锌矿床黏土矿物K-Ar测年及其地质意义[J].矿床地质,2005,24(3):317-324. Zhang Changqing,Mao Jingwen,Liu Feng,et al. K-Ar Dating of Altered Clay Minerals From Huize Pb-Zn Deposit in Yunnan Province and Its Geological Significance[J]. Mineral Deposits,2005,24(3):317-324.

[45] 李文博,黄智龙,王银喜,等.会泽超大型铅锌矿田方解石Sm-Nd等时线年龄及其地质意义[J].地质论评,2004,50(2):189-195. Li Wenbo,Huang Zhilong,Wang Yinxi,et al. Age of the Giant Huize Zn-Pb Deposit Determined by Sm-Nd Dating of Hydrothermal Calcite[J]. Geological Reriew,2004,50(2):189-195.

[46] 张云新,吴越,田广,等.云南乐红铅锌矿床成矿时代与成矿物质来源:Rb-Sr和S同位素制约[J].矿物学报,2014,34(3):305-311. Zhang Yunxin,Wu Yue,Tian Guang,et al. Mineralization Age and Source of Ore-Forming Material at Lehong Pb-Zn Deposit,Yunnan Province:Constraints From Rb-Sr and S Isotopes System[J]. Acta Mineralogica Sinica,2014,34(3):305-311.

[47] 韩奎,罗金海,王宗起,等.川滇黔交界地区铅锌矿床含矿角砾岩特征及其构造意义[J].矿床地质,2012,31(3):629-641. Han Kui,Luo Jinhai,Wang Zongqi. Feature of Ore-Bearing Breccias of Lead-Zinc Deposits in Sichuan-Yunnan-Guizhou Border Area and Its Tectonic Significance[J]. Mineral Deposits,2012,31(3):629-641.

[48] 刘家铎,张成江,刘显凡,等.扬子地台西南缘成矿规律及找矿方向[M].北京:地质出版社,2004:159-163. Liu Jiaduo,Zhang Chengjiang,Liu Xianfan,et al. Metallogenic Regularity and Prospecting in Southwestern Yangtze Massif[M]. Beijing:Geologyical Publishing House,2004:159-163.

[49] 杨永强,翟裕生,侯玉树,等.沉积岩型铅锌矿床的成矿系统研究[J]. 地学前缘,2006,13(3):200-205. Yang Yongqiang,Zhai Yusheng,Hou Yushu,et al. Study of Metallogenic System of Sediment-Hosted Lead and Zinc Deposits[J]. Earth Science Frontiers,2006,13(3):200-205.
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