Xi'an Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2019 Vol. 52, No. 4
Article Contents
Article navigation > Northwestern Geology > 2019 > 52(4): 1-13
Next Article Previous Article

ZHAO Pengbin, LI Weicheng, LUO Qianzhou, PENG Hailian, LI Yi, LI Wujie, ZHANG Shuanhou. 2019. Formation Age and Tectonic Environment of Yingzuihongshan Granite in Beishan, Inner Mongolia. Northwestern Geology, 52(4): 1-13.
Citation: ZHAO Pengbin, LI Weicheng, LUO Qianzhou, PENG Hailian, LI Yi, LI Wujie, ZHANG Shuanhou. 2019. Formation Age and Tectonic Environment of Yingzuihongshan Granite in Beishan, Inner Mongolia. Northwestern Geology, 52(4): 1-13.
shu

Formation Age and Tectonic Environment of Yingzuihongshan Granite in Beishan, Inner Mongolia

  • 1. School of Earth Science and Resources, China University of Geosciences(Beijing), Beijing 100083, China;

  • 2. Shaanxi Mineral Resources and Geological Survey, Xi'an 710054, Shaanxi, China

More Information
Received Date:  05 February 2019
Revised Date:  27 July 2019
    Abstract
  • Yingzuihongshan pluton is located at the eastern part of Beishan metallogenic belt in western Inner Mongolia, which is mainly consists biotite monzonite, porphyritic biotite monzonite and potassic granite. Previous studies have different views on the formation age of the rock mass, that is, it was formed in Silurian or Devonian. In this paper, the LA-ICP-MS zircon U-Pb dating of porphyritic biotite monzogranite obtains an age data of (423.1±1.5) Ma, indicating that the formation age of monzogranite was formed in Middle Silurian. Yingzuihongshan pluton belongs to calc-alkaline-high potassium calc-alkaline, peraluminous rock series. In primitive mantle normalized spider diagram, the samples are enriched in large ions lithophile elements (Rb, Th, K), while they are depleted in high field strength elements (Ta, Nb, Zr, Ti), with relatively enriched Hf. These rocks are characterized by LREE enrichment and depleted HREE, with obvious Eu anomaly and "right-deviation" REE distribution. Based on the testing data and some previous research results, it's suggested that Yingzuihongshan granite was formed by partial melting of lower crust during the collision stage of continental blocks.
    • FullText(HTML)
  • 加载中
    • References
  • 戴霜,方小敏,张翔,等.塔里木-中朝板块北缘志留纪岛弧公婆泉群火山岩地质地球化学及构造意义[J].兰州大学学报, 2003,39(04):80-87.

    Google Scholar

    DAI Shuang,FANG Xiaomin,ZHANG Xiang,et al. Island arc north of the Tarim-SK plate:the geology and geochemistry of Gongpoquan Group[J]. Journal of Lanzhou University(Natural Sciences), 2003,39(04):80-87.

    Google Scholar

    白大明,刘光海,常忠耀.甚低频电磁法在老硐沟氧化淋滤型金矿勘查中的应用效果[J].地质与勘探,1998,34(02):48-51.

    Google Scholar

    BAI Daming,LIU Guanghai,CHANG Zhongyao. Exploration of oxidizing-leaching type gold deposit of Laodonggou by Vlf-em method[J]. Geology and Exploration,1998,34 (02):48-51.

    Google Scholar

    丁嘉鑫,韩春明,肖文交,等.北山造山带花牛山岛弧东段钨矿床成矿时代和成矿动力学过程[J].岩石学报,2015,31(2):594-616.

    Google Scholar

    DING Jiaxin,HAN Chunming,XIAO Wenjiao,et al. Geochemistry and U-Pb geochronology of tungsten deposit of Huaniushan island arc in the Beishan Orogenic Belt,and its geodynamic background[J]. Actor Petrologica Sinica,2015,31(2):594-616.

    Google Scholar

    龚全胜,刘明强,李海林,等.甘肃北山造山带类型及基本特征[J].西北地质, 2002,35(3):28-34.

    Google Scholar

    GONG Quansheng,LIU Mingqiang,LI Hailin,et al. The Type and Basic Charac-teristics of Beishan Orogenic Belt, Gansu[J]. Northwestern Geology,2002,35(3):28-34.

    Google Scholar

    龚全胜, 刘明强, 梁明宏,等.北山造山带大地构造相及构造演化[J]. 西北地质, 2003,36(1):11-17.

    Google Scholar

    GONG Quansheng,LIU Mingqiang,LIANG Minghong,et al. The tectonic facies and tectonic evolution of Beishan orogenic belt,Gansu[J].Northwestern Geology, 2003,36(1):11-17.

    Google Scholar

    何世平, 任秉琛, 姚文光,等.甘肃内蒙古北山地区构造单元划分[J].西北地质, 2002,35 (4):30-40.

    Google Scholar

    HE Shiping, REN Bingchen, YAO Wenguang, et al. The Division of Tectonic Units of Beishan Area, Gansu-Inner Mongolia[J]. Northwestern Geology, 2002,35(4):30-40.

    Google Scholar

    何世平,周会武,任秉琛,等.甘肃内蒙北山地区古生代地壳演化[J].西北地质, 2005,38(3):6-15.

    Google Scholar

    HE Shiping, ZHOU Huiwu, REN Bingchen,et al. Crustal Evolution of Palaeozoic in Beishan Area, Gansu and Inner Mongolia, China[J]. Northwestern Geology, 2005,38(3):6-15.

    Google Scholar

    侯青叶,王忠,刘金宝,等.北山月牙山蛇绿岩地球化学特征及SHRIMP定年[J].现代地质, 2012,26(05):1008-1018.

    Google Scholar

    HOU Qingye, WANG Zhong, LIU Jinbao, et al. Geochemistry Characteristics and SHRIMP Dating of YueyashanOphiolite in Beishan Orogen[J].Geoscience, 2012,26(05):1008-1018.

    Google Scholar

    胡新茁,赵国春,胡新悦,等.内蒙古北山地区月牙山蛇绿质构造混杂岩带地质特征、形成时代及大地构造意义[J].地质通报, 2015,34(Z1):425-436.

    Google Scholar

    HU Xinzhuo, ZHAO Guochun, HU Xinyue,et al. Geological characteristics, formation epoch and geotectonic significance of the Yueyashan ophiolitic tectonic mélange in Beishan area, Inner Mongolia[J]. Geological Bulletin of China, 2015,34(Z1):425-436.

    Google Scholar

    黄典豪,王宝林.额济纳旗老硐沟氧化-淋滤型金矿床成矿特征[J].贵金属地质, 1997,6(02):13-20.

    Google Scholar

    HUANG Dianhao,WANG Baolin. Ore-forming characteristics of Laodonggouo xidized-leached type gold deposit in ejinaqi[J]. Journal of Precious Metallic Geology, 1997,6(02):13-20.

    Google Scholar

    李鹏, 吕新彪, 陈超,等.国庆钨矿钾长花岗岩年代学、地球化学特征及其地质意义[J]. 岩石矿物学杂志, 2011,30(1), 13-24.

    Google Scholar

    LI Peng,LÜ Xinbiao,CHEN Chao,et al. Chronology and geochemical characteristics of K-feldspar granite in the Gongqing tungsten deposit and their geological implications[J].Acta Petrologicaet Mineralogica, 2011,30(1), 13-24.

    Google Scholar

    李维成,赵鹏彬,罗乾周,等.内蒙古北山望旭山钨矿床地质特征与成矿时代约束[J].地质与勘探, 2018,54(04):659-673.

    Google Scholar

    LI Weicheng,ZHAO Pengbin,LUO Qianzhou,et al. Geological characteristics and mineralization age constraint of the Wangxushan tungsten deposit in Beishan,Inner Mongolia[J]. Geology and Exploration, 2018,54(04):659-673.

    Google Scholar

    刘夙明,刘雪刚.内蒙古凤凰山金矿床地质特征[J].新疆地质, 2007,25 (04):426-431.

    Google Scholar

    LIU Suming,LIU Xuegang. Geological features of fenghuangshan gold deposit in Neimengu[J]. Xinjiang Geology, 2007,25(04):426-431.

    Google Scholar

    聂凤军,江思宏.北山地区金属矿床成矿规律及找矿方向[M].北京:地质出版社,2002.

    Google Scholar

    NIE Fengjun, JIANG Sihong. Metallogenic Studies and Ore Prospecting in the Conjunction Area of Inner Mongolia Autonomous Region, Gansu Province and Xinjiang Uygur Autonomous Region (Beishan Mt.)[M]. Beijing:Geological Publishing House,2002.

    Google Scholar

    彭海练,杨克俭,李宁,等.内蒙古红石山南金矿地质特征及找矿方向[J].西北地质, 2011,44(4):44-49.

    Google Scholar

    PENG Hailian,YANG Kejian,LI Ning,et al. Geological Characteristics and Prospecting Direction of Gold Deposit in Southern Belt of Hongshishan, Ejinaqi, Inner Mongolia[J].Northwesten Geology, 2011,44(4):44-49.

    Google Scholar

    任秉琛,何世平,姚文光,等.甘肃北山牛圈子蛇绿岩铷-锶同位素年龄及其大地构造意义[J]. 西北地质, 2001,34(2):21-27.

    Google Scholar

    REN Bingchen,HE Shiping,YAO Wenguang,et al. Rb-Sr isotope age of Niuquanzi ophiolite and its tectonic significance in Beishan district,Gansu[J]. Northwestern Geology, 2001,34(2):21-27.

    Google Scholar

    彭海练,高峰,菅坤坤,等.内蒙古自治区额济纳旗红石山南二叠纪辉长岩体锆石U-Pb年龄及地质意义.矿产勘查, 2018(待出版).

    Google Scholar

    王国强.北山古生代蛇绿岩、火山岩研究与构造演化[D].长安大学,2015.

    Google Scholar

    WANG Guoqiang. The research of the Paleozoic ophiolites and volcanic rocks and the tectonic evolution in the Beishan area(Northwest China)[D].Chang'an University,2015.

    Google Scholar

    王国强,李向民,徐学义,等.甘蒙北山志留纪公婆泉群火山岩的地球化学及其对岩石成因和构造环境的制约[J].地质学报, 2016,90(10):2603-2619.

    Google Scholar

    WANG Guoqiang,LI Xiangmin,XU Xueyi.et al.Geochemistry of Gongpoquan Group in the Beishan Area,Gansu Province:Constraints on Petrogenesis and Tectonic Setting[J].Acta Geologica Sinaca, 2016,90(10):2603-2619.

    Google Scholar

    王盛栋.甘肃北山中部地区古生代洋板块地层重建与构造演化[D].中国地质大学(武汉),2017.

    Google Scholar

    WANG Shengdong. Reconstruction of Paleozoic Ocean Plate Stratigraphy in the middle Beishan Area, Gansu Province and its tectonic evolution[D]. China University of Geosciences (Wuhan),2017.

    Google Scholar

    王鑫玉.北山公婆泉岛弧岩石组合、岩浆时空演变及其构造意义[D].中国科学院大学(中国科学院广州地球化学研究所),2017.

    Google Scholar

    WANG Xinyu. The rock assemblages, spatial and temporal variations in the Gongpoquan arc, Beishan and their implications for tectonic setting[D]. Guangzhou Institute of Geochemistry, CAS,2017.

    Google Scholar

    武鹏,王国强,李向民,等.甘肃北山地区牛圈子蛇绿岩的形成时代及地质意义[J].地质通报, 2012,31(12):2032-2037.

    Google Scholar

    WU Peng,WANG Guoqiang,LI Xiangmin,et al. The age of Niujuanzi ophiolite in Beishan area of Gansu Province and its geological significance[J].Geological Bulletin of China, 2012,31(12):2032-2037.

    Google Scholar

    杨合群,李英,李文明,等.北山成矿构造背景概论[J].西北地质, 2008,41(1):22-28.

    Google Scholar

    YANG Hequn, LI Ying, LI Weming,et al. General discussion on metallogenitic tectonic setting of Beishan Mountain, northwestern China[J].Northwestern Geology, 2008,41(1):22-28.

    Google Scholar

    杨合群,李英,赵国斌,等.北山蛇绿岩特征及构造属性[J]. 西北地质, 2010a,43(1):26-36.

    Google Scholar

    YANG Hequn, LI Ying, ZHAO Guobin,et al.Character and Structural Attribute of the Beishan Ophiolite[J]. Northwestern Geology, 2010a,43(1):22-28.

    Google Scholar

    杨合群,赵国斌,李文明,等.内蒙古盘陀山一鹰嘴红山含钨花岗岩带形成时代及源区示踪[J].地质与勘探, 2010b,46(3):407-413.

    Google Scholar

    YANG Hequn, ZHAO Guobin, LI Wenming,et al. formation age and source tracing of the tungsten-bearing granite belt in the Pantuoshan-Yingzuihongshan area, Inner Mongolia[J]. Geology and Exploration, 2010b,46(3):407-413.

    Google Scholar

    杨合群,赵国斌,李英,等.新疆-甘肃-内蒙古衔接区古生代构造背景与成矿的关系[J].地质通报,2012,31(2/3):413-421.

    Google Scholar

    YANG Hequn,ZHAO Guobin, LI Ying, et al.The relationship betweenPaleozoic tectonic setting and mineralization in Xinjiang-Gansu-Inner Mongolia juncture area[J]. Geological Bulletin of China, 2012,31(2/3):413-421.

    Google Scholar

    于文松,廖昌溪,陈果.内蒙古老硐沟金矿床成因类型与找矿前景分析[J].黄金科学技术, 2013,21(02):24-27.

    Google Scholar

    YU Wensong,LIAO Changxi,CHEN Guo. Analysis of the Genetic Types and Prospect of Laodonggou Gold Deposit in Inner Mongolia[J]. Gold Science and Technology, 2013,21(02):24-27.

    Google Scholar

    赵国斌,李文明,杨合群,等.内蒙北山国庆钨矿床成矿特征与成因探讨[J]. 矿床地质, 2010,29(增刊):341-342.

    Google Scholar

    ZHAO Guobin,LI Wenming,YANG Hequn,et al. Geological and geochemical characteristics of the Guoqing tungsten deposit in Beishan Orogen,Inner Mongolia[J].Mineral Deposits, 2010,29(Suppl.):341-342.

    Google Scholar

    赵国斌,李文明,杨合群,等.内蒙古北山盘陀山钨矿床成矿特征及找矿标志[J].大地构造与成矿学,2013,37(02):235-241.

    Google Scholar

    ZHAO Guobin,LI Wenming,YANG Hequn,et al. Metallogenic Characteristics and Prospecting Indicators of the Pantuoshan Tungsten Deposit, Inner Mongolia, China[J].Geotectonica et Metallogenia,2013,37(02):235-241.

    Google Scholar

    赵鹏彬,付垒,高峰,等.内蒙古老硐沟钨矿床地质特征与找矿潜力分析[J]. 西部资源,2016(06):83-85.

    Google Scholar

    ZHAO Pengbin,FU Lei,GAO Feng,et al.2016.Geological Characteristics and prospecting potentiality of Laodonggou tungsten Desposit, Inner Mongolia[J].Westrn Resources,2016(06):83-85.

    Google Scholar

    郑荣国,吴泰然,张文,等.北山地区月牙山-洗肠井蛇绿岩的地球化学特征及形成环境[J].地质学报, 2012,86(06):961-971.

    Google Scholar

    ZHENG Rongguo,WU Tairan,ZHANG Wen,et al. Geochemical characteristics and tectonic setting and of the Yueyashan-Xichangjing Ophiolite in the Beishan area[J]. Acta Geologic Sinica,2012,86(06):961-971.

    Google Scholar

    周国庆,赵建新,李献华.内蒙古月牙山蛇绿岩特征及形成的构造背景:地球化学和Sr-Nd同位素制约[J]. 地球化学, 2000,29(2):108-119.

    Google Scholar

    ZHOU Guoqing,ZHAO Jianxin,LI Xianhua. Characteristics of the Yueyashan ophiolite from western Nei Mongol and its tectonic setting:Geochemistry and Sm-Nd isotopic constraints[J].Geochimica, 2000,29(2):108-119.

    Google Scholar

    左国朝,李茂松.甘蒙北山地区早古生代岩石圈形成和演化[M].兰州:甘肃科学技术出版社,1996.

    Google Scholar

    ZUO Guochao, LI Maosong. Fomation and Evolution of the Early Paleozoic Lithosphere in the Beishan Area,Gansu-Inner Mongolia,China[M]. Lanzhou:Gansu Science and Technology Press, 1996.

    Google Scholar

    左国朝,李绍雄.塔里木盆地东北缘早古生代构造格局及演化[J].中国地质, 2011,38(4):945-960.

    Google Scholar

    ZUO Guochao,LI Shaoxiong. Early Paleozoic tectonic framework and evolution in the northeast margin of Tarim Basin[J].Geology in China, 2011,38(4):945-960.

    Google Scholar

    AO SJ, XIAO WJ, HAN CM,et al. Geochronology and geochemistry of Early Permian mafic-ultramafic complexes in the Beishan area, Xinjiang, NW China:Implications for Late Paleozoic tectonic evolution of the southern Altaids[J]. Gondwana Research, 2010,18(2-3):466-478.

    Google Scholar

    FLOYD P A,WINCHESTER J A.Magma type and tectonic setting discrimination using immobile elements[J].Earth and Planetary Science Letters,1975,2(27):211-218. DOI:10.1016/0012-821X(75)90031-X.

    Google Scholar

    JACKSON S E, PEARSON N J, GRIFFIN W L,et al.The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology[J]. Chemical Geology, 2004, 211:47-69.

    Google Scholar

    LIU Y S, GAO S, HU Z C,et al. Continental and oceanic crust recy-cling-induced melt-peridotite interactions in the Trans-North Chi-na Orogenorogen:U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 2010, 51:537-571.

    Google Scholar

    LUDWIG K R. Isoplot/EX, version 3. A geochronological toolkit for Microsoft Excel[M].Berkeley Geochronology Center Special Publi-cations,2003.

    Google Scholar

    MANIA PD, PICCOLI PM.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin,1989,101(12):635-643. DOI:10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2.

    Google Scholar

    MIDDLEMOSTEAK. Magmas and Magmatic Rocks[M]. London:Longman,1985:1-266.

    Google Scholar

    PEARCE J A, HARRIS NBW,TINDLE AG. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology, 1984, 25(4):956-983.

    Google Scholar

    PECCERILLO A, TAYLOR SR. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions to Mineralogy and Petrology,1976, 58(1):63-81. DOI:10.1007/BF00384745.

    Google Scholar

    RUBATTO, DANIELA, GEBAUER, ET AL. Dieter Gebauer Usedse of cathodoluminescence for U-Pb zircon dating by ion microprobe:some examples from the western alps[M]. 2000,373-400.

    Google Scholar

    SLÁMA, J., J. KOŠLER, D. J. CONDON, J. L. Crowley,et al. Plesovice zircon-a new natural reference material for U-Pb and Hf isotopic microanaly-sis[J]. Chemical Geology, 2008, 249:1-35.

    Google Scholar

    XIAO W J, MAO Q G, WINDLEY B F, et al. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science,2010,310(10):1553-1594.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索
Export Citation
PDF
XML

Article Metrics

Article views(1668) PDF downloads(894) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020