Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (6): 1696-1710.doi: 10.13278/j.cnki.jjuese.20170228

Previous Articles    

Geological Significance and Metallogenic Epoch of the Baiyinnuoer Pb-Zn Deposit in Inner Mongolia: Constraints from Geochemistry and Chronology of Intrusive Rocks

Yang Fan1,2, Wang Yan1, Na Fuchao1, Fu Junyu1, Zhang Guangyu1, Sun Wei1, Pang Xuejiao1, Chen Jingsheng1, Liu Miao1, Li Bin1   

  1. 1. Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2017-09-11 Published:2018-11-26
  • Supported by:
    Supported by Project of China Geological Survey(DD20160048-1,DD20160343-08,DD20160048-16,DD20160201-01)

PDF (PC)

281

Abstract: Located in the south section of the Daxing'anling metallogenic belt, the Baiyinnuoer Pb-Zn deposit is a typical skarn deposit. In order to determine the mineralization age of the deposit, LA-ICP-MS U-Pb dating of zircons in the granodiorite porphyry and rhyolite porphyry associated with the mineralization was studied. The results suggest that the granodiorite and rhyolite porphyry were crystallized in (253.4±0.9) Ma and (133.6±0.7) Ma. The rock geochemistry indicates that the granodiorite is quasi-aluminous,and the rhyolite porphyry is excessive-aluminous. Both of them are characterized by fractionation of HREE and LREE, enrichment of large ion lithophile elements (LILE) and relative depletion of high field strength elements (HFSE). Combined with the geological characteristics and the previous research in this region, we conclude that two mineralization events occurred in the deposit with the early mineralization at about 253.4 Ma and the late one at about 133.6 Ma. The early mineralization may be related to the closure of the Paleo-Asian Ocean and the late mineralization was influenced by the subduction of the Mongolia-Okhotsk Ocean. The Baiyinnuoer Pb-Zn deposit was formed in the post-collisional extension.

Key words: skarn deposit, LA-ICP-MS zircon U-Pb chronology, intrusive rock, geochemistry, Baiyinnuoer Pb-Zn deposit, Inner Mongolia

CLC Number: 

  • P618.4
[1] 舒启海,赖勇,魏良民,等.大兴安岭南段白音诺尔铅锌矿矿床流体包裹体研究[J].岩石学报,2011,27(5):1467-1482. Shu Qihai, Lai Yong, Wei Liangmin, et al. Fluid Inclusion Study of the Baiyinnuoer Zn-Pb Deposit,South Segment of the Great Xing'an Mountain, Northeastern China[J]. Acta Petrologica Sinica, 2011, 27(5):1467-1482.
[2] 陈玉清,李长生,宋德奎.白音诺尔铅锌矿勘探类型及生产探矿[J].有色矿山,2002,31(3):16-18. Chen Yuqing, Li Changsheng, Song Dekui. Mineral Exploration Type and Productive Exploration in Baiyinnuoer Lead-Zinc Mine[J]. Nonferrous Mines, 2002, 31(3):16-18.
[3] 张德全,雷蕴芬,罗太阳.内蒙古白音诺尔铅锌矿床地质特征及成矿作用[J].矿床地质,1991,10(3):204-216. Zhang Dequan, Lei Yunfen, Luo Taiyang. Geological Characteristics and Metallogeny of the Baiyinnuoer Lead-Zinc Deposit, Inner Mongolia[J]. Mineral Deposits, 1991, 10(3):204-216.
[4] 曾庆栋,刘建明,贾长顺,等.内蒙古赤峰市白音诺尔铅锌矿沉积喷流成因:地质与硫同位素证据[J].吉林大学学报(地球科学版),2007,37(4):659-667. Zeng Qingdong, Liu Jianming, Jia Changshun, et al. Sedimentary Exhalative Origin of the Baiyinnuoer Zinc-Lead Deposit, Chifeng, Inner Mongolia:Geological and Sulfur Isotope Evidence[J]. Journal of Jilin University (Earth Science Edition), 2007, 37(4):659-667.
[5] 牛树银,孙爱群,郭立军,等.大兴安岭白音诺尔铅锌矿控矿构造研究与找矿预测[J].大地构造与成矿学,2008,32(1):72-80. Niu Shuyin, Sun Aiqun, Guo Lijun, et al. Ore-Control Structures and Prospecting for the Baiyinnuoer Pb-Zn Deposit in the Da Hinggan Range[J]. Geotection et Metalbgenia, 2008, 32(1):72-80.
[6] 江思宏,聂凤军,白大明,等.内蒙古白音诺尔铅锌矿铅同位素研究[J].地球科学与环境学报,2011,33(3):230-236. Jiang Sihong, Nie Fengjun, Bai Daming, et al. Study on the Lead Isotopic Features of the Baiyinnuoer Pb-Zn Deposit in Inner Mongolia[J]. Journal of Earth Sciences and Environment, 2011, 33(3):230-236.
[7] 易健,魏俊浩,姚春亮,等.内蒙古白音诺尔铅锌矿区三叠纪侵入岩体的发现及地质意义:锆石U-Pb年代学证据[J].地质科技情报,2012,31(4):10-16. Yi Jian, Wei Junhao, Yao Chunliang, et al. Discovery and Geological Significance of the Triassic Intrusive Rocks in the Baiyinnuoer Lead-Zinc Deposit, Inner Mongolia:Evidence from Zircon U-Pb Age[J]. Geological Science and Technology Information, 2012, 31(4):10-16.
[8] 王琦.内蒙古白音诺尔铅锌多金属矿床矽卡岩及含矿性研究[D].北京:北京大学,1991. Wang Qi. The Research on Skarn and Ore Poeentiality of Baiyinnuoer Pb-Zn Polymetallic Deposit[D]. Beijing:Peking University, 1991.
[9] 贾长顺,曾庆栋,徐九华,等.内蒙古白音诺尔铅锌矿褶皱控矿特征及找矿方向[J].北京科技大学学报,2008,30(4):331-338. Jia Changshun, Zeng Qingdong, Xu Jiuhua, et al. Characteristics of Ore-Controlling Folds and Orientatiion of Ore Prospecting in the Baiyinnuoer Lead-Zinc Deposit, Inner Mongolia[J].Journal of University of Science and Technology Beijing, 2008, 30(4):331-338.
[10] 曾庆栋,刘建明,万志民,等.内蒙古赤峰市白音诺尔铅锌矿床构造控制与找矿方向[J].大地构造与成矿学,2007,31(4):430-434. Zeng Qingdong, Liu Jianming, Wan Zhimin, et al. Structual Controls and Exploration Targets of the Baiyinnuoer Zinc-Lead Deposit, Chifeng, Inner Mongolia[J]. Geotection et Metalbgenia, 2007, 31(4):430-434.
[11] 江思宏,聂凤军,白大明,等.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据[J].矿床地质,2011,30(5):787-798. Jiang Sihong, Nie Fengjun, Bai Daming, et al. Geochronology Evidence for Indosinian Mineralization in Baiyinnuoer Pb-Zn Deposit of Inner Mongolia[J]. Mineral Deposits, 2011, 30(5):787-798.
[12] 李怀坤,耿建珍,郝爽,等.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J].矿物学报,2009,29(增刊1):600-601. Li Huaikun, Geng Jianzhen, Hao Shuang, et al. The Study of Zircon U-Pb Isotopic Age by Laser Ablation Multi-Collector Plasma Mass Spectrometry(LA-MC-ICPMS)[J].Acta Mineralogica Sinica, 2009, 29(Sup.1):600-601.
[13] Moeller A O,Brien P J, Kennedy A, et al.Linking Growth Episodes of Zircon and Metamorphic Textures to Zircon Chemistry:An Example from the Ultrahigh-Temperature Granulites of Rogaland,SW Norway[J].Geological Society Special Publications, 2003, 220:65-81.
[14] 吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604. Wu Yuanbao, Zheng Yongfei. The Study of Zircon Genesis Mineralogy and Constraints of the Interpretation on Its U-Pb Age[J]. Chinese Science Bulletin, 2004, 49(16):1589-1604.
[15] Rubatto D, Gebauer D.Use of Cathodoluminescence for U-Pb Zircon Dating by IOM Microprobe:Some Examples from the Western Alps[J].Cathodoluminescence in Geoscience, 2000, 49(16):1589-1604.
[16] 王京彬,王玉往,王莉娟.大兴安岭南段锡多金属成矿系列[J].地质与勘探.2005,41(6):15-20. Wang Jingbin, Wang Yuwang, Wang Lijuan. Tin-Polymetallicmetallogenic Serises in the Southern Part of Da Hinggan Mountains China[J]. Geology and Prospecting, 2005, 41(6):15-20.
[17] 邵济安,张履桥,牟保磊.大兴安岭中南段中生代的构造热演化[J].中国科学:D辑,1998,28(3):193-200. Shao Ji'an, Zhang Lüqiao, Mou Baolei. The Tectionic-Thermal Evolution of Southern-Middle Parts of the Da Hingganling Mountains[J]. Science in China:Series D, 1998, 28(3):193-200.
[18] 邵济安,张履桥,牟保磊.大兴安岭中生代伸展造山过程中的岩浆作用[J].地学前缘,1999,6(4):339-346. Shao Ji'an, Zhang Lüqiao, Mou Baolei. Magmatism in the Mesozoic Extending Orogenic Process of Da Hinggan Mts[J]. Earth Science Frontiers, 1999, 6(4):339-346.
[19] Ishiyama D, Sato R, Mizuta T, et al. Characteristic Features of Tin-Iron-Copper Mineralization in the Anle-Huanggangliang Mining Area, Inner Mongolia, China[J]. Resource Geology,2001, 51(4):377-392.
[20] Wang J B, Wang Y W, Wang L J, et al. Tin-Polymetallic Mineralization in the Southern Part of the Da Hinggan Mountains, China[J]. Resour Geol, 2001, 51(4):283-291.
[21] 张炯飞,朱群,武广,等.大兴安岭热液矿床成矿时代[J].矿床地质,2002,21(增刊):309-311. Zhang Jiongfei, Zhu Qun, Wu Guang, et al. On Metallogenetic Epoch of Hydrothermal Deposits in Da Hinggan Area[J].Mineral Deposits, 2002, 21(Sup.):309-311.
[22] Zhu X Q, Zhang Q, He Y L, et al. Hydrothermal Source Rocks of the Meng'entalegai Ag-Pb-Zn Deposit in the Granite Batholith, Inner Mongolia, China[J]. Geochemical Journal, 2006, 40(3):265-275.
[23] Zeng Q D,Liu J M,Zhang Z L,et al.Geologic,Fluid Inclusion and Sulfur Isotopic Studies of the Chehugou Porphyry Molybdenum-Copper Deposit,Xilamulun Metallogenic Belt,NE China[J].International Geology Review (in Review),2010, 46(2):1536-1548.
[24] Zeng Q D, Liu J M, Zhang Z L. Re-Os Geoch-ronology of Porphyry Molybdenum Deposit in South Segment of Da Hinggan Mountains, Northeast China[J]. Journal of Earth Science, 2010, 21(4):392-401.
[25] 周振华,吕林素,冯佳睿,等.内蒙古黄岗夕卡岩型锡铁矿床辉钼矿Re-Os年龄及其地质意义[J]. 岩石学报,2010, 26(3):667-679. Zhou Zhenhua, Lü Linsu, Feng Jiarui, et al. Molybdenite Re-Os Ages of Huanggang Skarn Sn-Fe Deposit and Their Geological Significance, Inner Mongolia[J].Acta Petrologica Sinica, 2010, 26(3):667-679.
[26] Liu Jianming, Jie Ye, Zhang Anli, et al. A New Exhalite Type Siderite-Sericite Chert Formed in Fault-Controlled Lacustrine Basin[J]. Science in China:Series D, 2001, 44:408-415.
[27] 王长明.大兴安岭中南段喷流-沉积成矿特征与成矿预测[D].北京:中国地质大学,2008. Wang Changming. The Jet-Sedimentary Metallogenic Characteristics and Prediction of Daxing'anling South Section[D]. Beijing:China University of Geosciences, 2008.
[28] 孙兴国.内蒙古龙头山Ag-Pb-Zn多金属矿床成矿模式及找矿模型[D].北京:中国科学院研究生院,2008. Sun Xingguo. The Metallogenic and Prospecting Model of Longtoushan Ag-Pb-Zn Polymetallic Deposit, Inner Mongolia[D]. Beijing:Graduate School of Chinese Academy of Sciences, 2008.
[29] Wan B,Ernst H,Zhang LC,et al. Rb-Sr Geochro-nology of Chalcopyrite from the Chehugou Porphyry Mo-Cu Deposit (Northeast China) and Geochemical Constraints on the Origin of Hosting Granites[J]. Economic Geology, 2009, 104:351-363.
[30] Zhang L C,Wu H Y, Wan B, et al. Ages and Geodynamic Settings of Xilamulun Mo-Cu Metallogenic Belt in North of North China Craton[J]. Gondwana Research,2009, 16:243-254.
[31] Liu J M,Zhao Y,Sun Y L, et al.Recognition of the Latest Permian to Early Triassic Cu-Mo Mineralization on the Northern Margin of the North China Block and Its Geological Significance[J]. Gondwana Research, 2010, 17(1):125-134.
[32] Zeng Q D, Liu J M, Chu S X, et al. Mesozoic Molybdenum Deposits in the East Xingmeng Orogenic Belt, Northeast China:Characteristics and Tectonic Setting[J]. International Geology Review, 2012, 47(3):1846-1862.
[33] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30.
[34] 张连昌,英基丰,陈志广,等.大兴安岭南段三叠纪基性火山岩时代与构造环境[J].岩石学报,2008, 24(4):911-921. Zhang Lianchang, Ying Jifeng, Chen Zhiguang, et al. Age and Tectonic Setting of Triassic Basic Volcanic Rocks in Southern Da Hinggan Range[J].Acta Petrologica Sinica, 2008, 24(4):911-921.
[35] 邵济安,赵国龙,王忠,等.大兴安岭中生代火山活动构造背景[J].地质论评,1999,45(增刊):422-430. Shao Ji'an, Zhao Guolong, Wang Zhong, et al. Tectonic Setting of Mesozoic Volcanism in Da Hinggan Mountains, Northeasertn China[J]. Geological Review, 1999, 45(Sup.):422-430.
[36] Zhang X H, Zhang H F, Zhai M G, et al. Geo-chemistry of the Middle Triassic Gabbros from the Northern Liaoning,North China:Origin and Tectonic Implications[J]. Geological Magazine,2009,140:540-551.
[37] Zhang S H, Zhao Y, Liu X C, et al. Late Paleozoic to Early Mesozoic Mafic-Ultramafic Complexes from the Northern North China Block:Constraints on the Composition and Evolution of the Lithospheric Mantle[J]. Lithos, 2009, 110(1):229-246.
[38] 张连昌,吴英华,相鹏,等.中生代复杂构造体系的成矿过程与成矿作用:以华北大陆边缘西拉木伦钼铜多金属成矿带为例[J].岩石学报,2010,26(5):1351-1362. Zhang Lianchang, Wu Yinghua, Xiang Peng, et al. Ore-Forming Processes and Mineralization of Complex Tectonic System During the Mesozoic:A Case from Xilamulun Cu-Mo Metallogenic Belt[J]. Acta Pertologica Sinica, 2010, 26(5):1351-1362.
[39] 欧阳荷根.大兴安岭南段拜仁达坝-维拉斯托银多金属矿床成矿作用及动力学背景[D].北京:中国地质大学,2013. Ouyang Hegen. Metllogenesis of Bairendaba-Weilasituo Silver-Polytmetallic Deposit and Its Geodynamic Setting, in the Southern Segment of Great Xing'an Gange, NE China[D]. Beijing:China University of Geosciences, 2013.
[40] 李锦轶,高立明,孙桂华,等.内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J].岩石学报,2007,23(3):565-582. Li Jinyi, Gao Liming, Sun Guihua, et al. Shuangjingzi Middle Triassic Syn-Collisional Crust-Derived Granite in the East Inner Mongolia and Its Constraint on the Timing of Collision Between Siberian and Sino-Korean Paleo-Plates[J],Acta Petrologica Sinica, 2007, 23(3):565-582.
[41] Pitcher W S. Granite Type and Tectonic Environment[C]//Hsu K.Mountain Building Processes.London:Academic Press, 1983:19-40.
[42] Wang T, Zheng Y D, Zhang J J, et al. Pattern and Kinematic Polarity of Late Mesozoic Extension in Continental NE Asia:Perspectives from Metamorphicn Corecomplexes[J]. Tectonics, 2011, 30(6):896-913.
[43] Wu F Y, Sun D Y, Li H M, et al. A-Type Granites in Northeastern China:Age and Geochemical Constraints on Their Petrogenesis[J].Chemical Geology, 2002, 187(1/2):143-173.
[44] Wang T, Guo L, Zheng Y D, et al. Timing and Processes of Late Mesozoic Mid-Lower-Crustal Extension in Continental NE Asia and Implications for the Tectonic Setting of the Destruction of the North China Craton:Mainly Constrained by Zircon U-Pb Ages from Metamorphic Core Complexes[J]. Lithos, 2012, 154:315-345.
[45] Wang F, Zhou X H, Zhang L C, et al. Late Mesozoic Volcanism in the Great Xing'an Range (NE China):Timing and Implications for the Dynamic Setting of NE Asia[J]. Earth and Planetary Science Letters, 2006, 251(1):179-198.
[46] Wu F Y, Lin J Q, Wilde S A, et al. Nature and Significance of the Early Cretaceous Giant Igneous Event in Eastern China[J]. Earth and Planetary Science Letters, 2005, 233(1):103-119.
[47] Meng Q R. What Drove Late Mesozoic Extension of the Northern China-Mongolia Tract?[J]Tectonophysics, 2003, 369(3/4):155-174.
[1] Lü Junchao, Shu Guanglong, Zhang Debao, Zhao Yan, Liu Guixiang, Bi Zhongwei. Geochronology and Metallogenic Epoch of Shenshan Fe-Cu Deposit in Zhalaite County, Inner Mongolia and Its Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(6): 1683-1695.
[2] Zhang Qiang, Ding Qingfeng, Song Kai, Cheng Long. Detrital Zircon U-Pb Geochronology and Hf Isotope of Phyllite of Langyashan Formation in Hongshuihe Iron Ore District of Eastern Kunlun and Their Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1085-1104.
[3] Cui Yachuan, Yu Jiejiang, Yang Wanzhi, Zhang Yuanhou, Cui Ce, Yu Jielu. Geochronology, Geochemistry and Petrogenesis of Hornblende Gabbro in Huangshan Area of Jueluotage Belt, Eastern Tianshan [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1105-1120.
[4] Guo Chuntao, Li Ruyi, Chen Shumin. Rare Earth Element Geochemistry and Genetic Model of Dolomite of Yingshan Formation in Gucheng Area, Tarim Basin [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1121-1134.
[5] Zhao Xilin, Jiang Yang, Xing Guangfu, Yu Shengyao, Peng Yinbiao, Huang Wencheng, Wang Cunzhi, Jin Guodong. Chencai Early Paleozoic Subduction-Accretionary and Their Restrictions on Collage Between Cathaysia and Yangtze Block [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1135-1153.
[6] Wang Chaoyang, Meng En, Li Zhuang, Li Yanguang, Jin Mengqi. Age, Petrogenesis and Their Constraints on Regional Crustal Evolution of Late Neoarchean Gneisses in Southeast Jilin Province [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(3): 587-625.
[7] Qi Tianjiao, Xue Chunji, Xu Bixia. Zircon U-Pb Age and Geochemical Characteristics of Granites from Buheta Cu(Au) Mineralization District in Zhaosu County, Xinjiang Province [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(1): 132-144.
[8] Sun Fanting, Liu Chen, Qiu Dianming, Lu Qian, He Yunpeng, Zhang Mingjie. Petrogenesis and Geodynamic Significance of Intermediate-Basic Intrusive Rocks in Xiaokuile River, Eastern Slope of the Great Xing'an Range: Evidences of Zircon U-Pb Geochronology, Elements and Hf Isotope Geochemistry [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(1): 145-164.
[9] Ruan Dawei, Li Shunda, Bi Yaqiang, Liu Xingyu, Chen Xuhu, Wang Xingyuan, Wang Keyong. Ore-Controlling Structures and Deep Metallogenic Prediction of Aerhada Pb-Zn Deposit in Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1705-1716.
[10] Zhang Chao, Cui Fanghua, Zhang Zhaolu, Geng Rui, Song Mingchun. Petrogenesis of Ore-Bearing Dioritic Pluton in Jinling Area in Western Shandong:Evidence from Zircon U-Pb Chronology and Petro-Geochemistry [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1732-1745.
[11] Shi Ke, Zhang Dayu, Ding Ning, Wang Deen, Chen Xuefeng. Geochronology, Geochemistry and Formation of Xiaoyao Rock in Southern Anhui Province [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1746-1762.
[12] Wang Shijie, Xu Zhongyuan, Dong Xiaojie, Du Yang, Cui Weilong, Wang Yang. Permian Tectonic Evolution of the Middle Section of Northern Margin of the North China Plate:Constraints from Zircon U-Pb Geochronology and Geochemistry of the Volcanic Rocks [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(5): 1442-1457.
[13] Xu Zhongjie, Lan Yizhi, Cheng Rihui, Li Shuanglin. Carbonate Geochemical Record of Sea-Level Change of Lunshan Formation in Lower Ordovician in Jurong Area [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(5): 1458-1470.
[14] Zhao Yuandong, Che Jiying, Wu Datian, Xu Fengming, Zhao Jun, Li Shichao. Early-Middle Jurassic TTG Granites in Northwest of Lesser Xing'an Range: Its Geochronology, Geochemical Characteristics and Tectonic Significance [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(4): 1119-1137.
[15] Liu Chen, Sun Jinggui, Qiu Dianming, Gu Alei, Han Jilong, Sun Fanting, Yang Mei, Feng Yangyang. Genesis and Geological Significance of Mesozoic Volcanic Rocks in Xiaomoerke, Northern Slope of Greater Khingan Range: Hf Isotopic Geochemistry and Zircon U-Pb Chronology [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(4): 1138-1158.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
Copyright © Journal of Jilin University(Earth Science Edition), All Rights Reserved.
Tel: +86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
Powered by Beijing Magtech Co. Ltd