吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (6): 1740-1753.doi: 10.13278/j.cnki.jjuese.201606112

• 地质与资源 • 上一篇    下一篇

赤峰撰山子花岗岩年代学、地球化学特征及其成岩动力学背景

孙珍军1, 孙国胜2, 于赫楠1, 向柱1, 田毅3, 刘彤4, 陈旭4, 李杨4   

  1. 1. 防灾科技学院地震科学系, 北京 101601;
    2. 吉林大学地球科学学院, 长春 130061;
    3. 辽宁省地质矿产调查院, 沈阳 110031;
    4. 核工业二四三大队, 内蒙古 赤峰 024006
  • 收稿日期:2016-04-25 出版日期:2016-11-26 发布日期:2016-11-26
  • 通讯作者: 孙国胜(1964-),男,副教授,主要从事矿床地球化学研究,E-mail:sgsh8888@163.com E-mail:sgsh8888@163.com
  • 作者简介:孙珍军(1982-),男,讲师,主要从事矿床学研究,E-mail:306292193@qq.com
  • 基金资助:
    河北省高等学校科学技术研究重点项目（ZD2015203）；中央高校基本科研业务费资助项目（ZD2015203）

Chronology and Geochemical Characteristics of Zhuanshanzi Granite in Chifeng and Its Diagenetic Dynamics Background

Sun Zhenjun1, Sun Guosheng2, Yu Henan1, Xiang Zhu1, Tian Yi3, Liu Tong4, Chen Xu4, Li Yang4   

  1. 1. Department of Earthquake Science, Institute of Disaster Prevention Science and Technology, Beijing 101601, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. Liaoning Survey Academy of Geology and Mineral Resources, shenyang 110031, China;
    4. 243 Team of Nuclear Industry, Chifeng 024006, Inner Mongolia, China
  • Received:2016-04-25 Online:2016-11-26 Published:2016-11-26
  • Supported by:
    Supported by Higher School Science and Technology Research Key Project in Hebei Province(ZD2015203) and Central University Basic Scientific Research Business Expenses Funded Project(ZD2015203)

PDF (PC)

470

摘要： 撰山子角闪二长花岗岩位于华北克拉通与兴蒙造山带结合部位的中生代构造岩浆活动带，对其开展了主量元素、稀土和微量元素分析以及LA-ICP-MS锆石U-Pb定年等工作，目的在于精确厘定岩体的形成时代和研究其形成的动力学背景。结果表明：花岗岩的LA-ICP-MS锆石U-Pb谐和年龄为（245.8±3.1）Ma（MSWD=3.7，n=17），属早三叠世。岩石地球化学成分特征显示为，其具有高硅（w（SiO2）=71.68%~72.85%）、富碱（w（Na2O+K2O）=8.98%~9.20%）、高铝（w（Al2O3）=13.45%~13.77%）、低钙（w（CaO）=0.81%~0.99%）及低TFeO/MgO值（平均值为6.55）的特征，属高钾钙碱性、高分异I型弱铝质花岗岩；稀土配分曲线呈现向右倾斜的配分模式，Eu具有明显的亏损（δEu=0.66~0.68），表明斜长石发生了明显的分离结晶作用；在微量元素原始地幔标准化图谱上呈现清晰的Th、U、La、P富集，Ba、Nb、Ti、Sr、Ta等相对亏损的特征。综合分析认为，撰山子角闪二长花岗岩主要形成于下地壳部分熔融作用，可能有少量的地幔组分加入，其形成于华北板块和西伯利亚板块最终拼合后的后碰撞/后造山伸展作用构造环境。

关键词: 花岗岩, 地球化学, LA-ICP-MS锆石U-Pb定年, 构造环境, 撰山子

Abstract: The Zhuanshanzi hornblende monzogranite is located in the the Mesozoic tectonic magmatic active belt which between the North China craton and the Xingmeng orogeny belt. Testing of major elements, rare-earth elements (REEs), trace elements and LA-ICP-MS zircon U-Pb dating of the hornblende monzogranite have be carried out to accurately determined the forming age and study the dynamics background of the granite,rock. Results show that the LA-ICP-MS zircon U-Pb age of the hornblende monzogranite is (245.8±3.1) Ma. (MSWD=3.7,n=17), and belongs to the Early Triassic. Geochemically, the granite is characterized by high concentrations of silica (w(SiO2)=71.68%-72.85%), alkali (w(Na2O+K2O)=8.98%-9.20%), and alumina (w (Al2O3)=13.45%-13.77%); low concentrations of calcium (w(CaO)=0.81%-0.99%); and with low values of TFeO/MgO (average is 6.55), indicating the hornblende monzogranite belongs to high-K, calc-alkaline high differentiation Ⅰ type, weak aluminum granite. The granite is enriched in LREE and relatively depleted in HREE(LaN/YbN=21.94-24.33), and obvious Eu anomaly (δEu=0.66-0.68), which indicates that a large number of the plagioclase fractionation occured during the magmatic processes. In addition, the granite is enriched in Th, U, La and P, and depleted in Ba, Nb, Ti, Sr and Ta, and so on. In summary, the Zhuanshanzi granite is mainly formed by partial melting of crust material, with a few new mantle source composition. It is formed under the extensional tectonic setting in post-collision or post-orogenic stage after the North China plate and Siberia plate's eventual collision.

Key words: granite, geochemistry, LA-ICP-MS zircon U-Pb dating, tectonic setting, Zhuanshanzi

中图分类号: 

  • P588.12
[1] Jian Ping, Liu Dunyi, Kroner A, et al. Time Scale of an Early to Mid-Paleozoic Orogenic Cycle of the Long-Lived Central Asian Orogenic Belt, Inner Mongolia of China: Implications for Continental Growth[J]. Lithos, 2008, 101(3): 233-259.
[2] 陈衍景,翟明国,蒋少涌. 华北大陆边缘造山过程与成矿研究的重要进展和问题[J]. 岩石学报,2009, 25(11): 2695-2726. Chen Yanjing, Zhai Mingguo, Jiang Shaoyong. SignificantAchievements and Open Iissues in Study of Orogenseis and Metallagenesis Surrounding the North China Continent[J]. Acta Petrologica Sinica, 2009, 25(11): 2695-2726.
[3] 王荃,刘雪亚,李锦轶. 中国华夏与安加拉古陆间的板块构造[M].北京:北京大学出版社,1991: 56-60. Wang Quan, Liu Xueya, Li Jinyi.Plate Tectonics Between Cathaysia and Angaraland in China[M]. Beijing: Peking University Press, 1991:56-60.
[4] 邵济安. 中朝板块北缘中段地壳演化[M]. 北京:北京大学出版社,1991:1-136. Shao Ji'an. Evolution of Crust in the Middle of Northern Sino-Korean Plate[M]. Beijing: Peking University Press, 1991:1-136.
[5] Sengor A M C,Natal'In B A, Burtman V S. Evolution of the Altaid Tectonic Collage and Paleozoic Crustal Growth in Eurasia[J]. Nature, 1993,364(6435): 299-307.
[6] Xiao Wenjiao, Windley B F, Badarch G,et al. Paleozoic Accretionary and Convergent Tectonics of the Southern Altaids: Implications for the Growth of Central Asia[J]. Journal of the Geological Society, 2004,161(3):339-342.
[7] Xiao Wenjiao, Windley B F, Huang Baochun,et al. End-Permian to Mid-Triassic Termination of the Accretionary Processes of the Southern Altaids: Iimplications for the Geodynamic Evolution, Phanerozoic Continental Growth, and Metallogeny of Central Asia[J]. International Journal of Earth Sciences, 2009, 98: 1189-1217.
[8] Xiao Wenjiao, Windley B F, Hao Jie, et al. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China: Termination of the Central Asian Oragenic Belt[J]. Tectonics, 2003, 22(6): 1-8.
[9] Yakubchuk A. Architecture and Mineral Deposit Se-ttings of the Altaid Orogenic Collage: A Revised Model[J]. Journal of Asian Earth Sciences, 2004, 23(5): 761-779.
[10] Hong Dawei, Zhang J S,Wang T, et al. Continental Crus-tal Growth and the Supercontinental Cycle: Evidence from the Central Asian Orogenic Belt[J]. Journal of Asian Earth Sciences, 2004, 23(5): 799-813.
[11] Jahn B M,Wu Fuyuan, Hong Dawei. Important Crus-tal Growth in the Phanerozoic: Isotopic Evidence of Granitoids from East-central Asia[J]. Proceedings of the Indian Academy of Sciences (Earth and Planetary Sciences), 2000,109(1): 5-20.
[12] Jahn B M. Phanerozoic Continental Growth in Central Asia[J]. Journal of Asian Earth Sciences, 2004, 23(5): 599-603.
[13] Yang Jinhui, Chung S L, Zhai Mingguo, et al., Geo-chemical and Sr-Nd-Pb Isotopic Compositions of Mafic Dikes from the Jiaodong Peninsula, China: Evidence for Vein-Plus-Peridotite Melting in the Lithospheric Mantle[J]. Lithos, 2004, 73(3/4):145-160.
[14] Liu Wei,Siebel W,Li Xinjun, et al. Petrogenesis of the Linxi Granitoids, Northern Inner Mongolia of China: Constraints on Basaltic Underplating[J]. Chemical Geology, 2005, 219(1/2/3/4): 5-35.
[15] Zhang Shuanhong, Zhao Yue, Song Biao,et al. Car-boniferous Granitic Plutons from the Northern Margin of the North China Block: Implications for a Late Paleozoic Active Continental Margin[J]. Journal of the Geological Society London, 2007, 164: 451-463.
[16] Kusky T M, Windley B F, Zhai Mingguo. Tectonic Evolution of the North China Block: From Orogen to Craton to Orogen[C]//Zhai Mingguo, Windley B F, Kusky T, et al.Mesozoic Subcontinental Thinning Beneath Easten North China. London: Geological Society Special Publication, 2007: 1-34.
[17] 孙德有,吴福元,张艳斌,等. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间: 来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版),2004, 34(2): 174-181. Sun Deyou, Wu Fuyuan, Zhang Yanbin, et al. The Final Closing Time of the West Lamulun River-Changchun-Yanji Plate Suture Zone-Evidence from the Dayushan Granitic Pluton,Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 2004, 34(2): 174-181.
[18] Wu Fuyuan, Sun Deyou, Jahn B M, et al. A Jurassic Garnet-Bearing Granitic Pluton from NE China Showing Tetrad REE Patterns[J]. Asian Earth Sci, 2004, 23: 731-744.
[19] 李锦轶,高立明,孙桂华. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩及其对西伯利亚与中朝古板块碰撞时限的约束的确定[J]. 岩石学报,2007,23(3):565-582. Li Jinyi,Gao Liming,Sun Guihua. Shuangjingzi Middle Triassic Syn-Collislonal 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 Sinaica, 2007, 23(3): 565-582.
[20] 李锦轶,张进,杨天南,等. 北亚造山区南部及其毗邻地区地壳构造分区与构造演化[J]. 吉林大学学报(地球科学版),2009,39(4): 584-605. Li Jinyi, Zhang Jin, Yang Tiannan, et al. Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas[J]. Journal of Jilin University (Earth Science Edition), 2009,39(4): 584-605.
[21] 李益龙,周汉文,钟增球. 华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石LA-ICP-MS U-Pb年龄证据[J]. 地球科学:中国地质大学学报,2009,34(6):931-938. Li Yilong,Zhou Hanwen,Zhong Zengqiu. Collision Processes of North China and Siberian Plates:Evidence from LA-ICP-MS Zircon U-Pb Age on Deformed Granite in Xar Moron Suture Zone[J]. Earth Science:Journal of China University of Geosciences, 2009,34(6): 931-938.
[22] Li Jinyi. Peimina Geodynamic Setting of Northeast China and Adjacent Regions: Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26: 207-224.
[23] 孙珍军. 华北克拉通北缘赤峰-朝阳地区金矿成矿作用研究[D]. 长春:吉林大学, 2013:1-194. Sun Zhenjun. Study on Gold Deposits Mineralization in Chifeng-Chaoyang Region,Northern Margin of North China Craton[D]. Changchun: Jilin University, 2013:1-194.
[24] 刘建峰,迟效国,赵芝,等. 内蒙古巴林右旗建设屯埃达克岩锆石U-Pb年龄及成因讨论[J]. 岩石学报,2013, 29(3): 827-839. Liu Jianfeng, Chi Xiaoguo, Zhao Zhi, et al.Zircon U-Pb Age and Petrogenetic Discussion on Jianshetun a Dakite in Balinyouqi, Inner Mongolia[J]. Acta Petrologica Sinica, 2013, 29(3): 827-839.
[25] Prelevi? D, Foley S F, Cvetkovi? V, et al. Origin of Mine tte by Mixing of Lamproite and Dacite Magmas in Veliki Majdan, Serbia[J]. Journal of Petrology, 2004, 45(4): 759-792.doi:10.1093/petrology/egg109.
[26] Tan Jun, Wei Junhao, Guo Lingli, et al. LA-ICP-MS Zircon U-Pb Dating and Phenocryst EPMA of Dikes, Guocheng, Jiaodong Peninsula:Implications for North China Craton Lithosphere Evolution[J]. Science in China:Series D, 2008, 51(10):1483-1500.doi:10.1007/s11430-008-0079-3.
[27] 付乐兵,魏俊浩,魏启荣,等.内蒙古金厂沟梁地区晚三叠世脉岩地球化学特征及成岩动力学背景[J]. 地球科学:中国地质大学学报,2010, 35(6): 933-946. Fu Lebing, Wei Junhao, Wei Qirong, et al. Petrogenesis and Geodynamic Setting of Late Triassic Dykes of Jinchanggouliang, Eastern Inner Mongolia[J]. Earth Science:Journal of China University of Geosciences, 2010, 35(6): 933-946.
[28] 吴利仁,李秉伦.中国东部中生代两大类斑岩型矿床[M]. 北京:科学出版社,1991:1-318. Wu Liren, Li Binglun. Two Kinds Big Porphyry Deposits in the Mesozoic of Eastern China[M]. Beijing: Science Press, 1991:1-318.
[29] 邵济安,刘福田,陈辉,等. 大兴安岭-燕山晚中生代岩浆活动与俯冲作用的关系[J]. 地质学报,2001, 75(1): 56-63. Shao Ji'an, Liu Futian,Chen Hui,et al. Relationship Between Mesozoic Magmatism and Subduction in Da Hinggn-Yanshan Area[J]. Acta Geologica Sinica, 2001, 75(1): 56-63.
[30] 苗来成,范薇茗,翟明国,等. 金厂沟梁-二道沟金矿田内花岗岩类侵入体锆石的离子探针U-Pb年代学及意义[J]. 岩石学报, 2003, 19(1): 71-80. Miao Laicheng,Fan Weiming,Zhai Mingguo,et al. Zircon SHRIMP U-Pb Geochronology of the Granitold Iintrusions from Jinchanggouliang-Erdaogou Gold Oreflied and Its Singnificance[J]. Acta Petrologica Sinaica, 2003, 19(1): 71-80.
[31] 李永刚,翟明国,杨进辉,等. 内蒙古赤峰安家营子金矿成矿时代以及对华北中生代爆发成矿的意义[J]. 中国科学:D辑,2003,33(10):960-965. Li Yonggang, Zhai Mingguo, Yang Jinhui, et al. Significanceog the Outbreak of Mesozoic Metallogenic and Gold Metallogenic Epoch in Inner Mongolia Chifeng Anjiayingzi[J]. Science in China:Series D, 2003,33(10):960-965.
[32] 李秀琴, 杨吉. 内蒙撰山子金矿赋存规律及成矿预测[J]. 长春科技大学学报, 2000,30(1):33-36. Li Xiuqin, Yang Ji.Occurrence Regularity and Metallogetic Progenosis of Zhuanshanzi Gold Deposit, Inner Mongolia[J]. Journal of Changchun University of Science and Technology, 2000,30(1):33-36.
[33] Yuan Honglin,Gao Shan,Liu Xiaoming, et al. Accu-ratee U-Pb Age and Trace Element Deteminations of Zircon by Laser Ablation-Inductively Coupled Plasma Mass Spectrometry[J]. Geosand News, 2004, 28(3): 353-370.
[34] Williams,Claesson.Isotopic Evidence for the Precam-brian Provenance and Caledonian Metamorphism of High Grade Paragneisses from the Seve Nappes,Scandinavian Caledonides[J].Contrib Mineral Petrol,1987,97(2):205-217.
[35] Sun S S,McDonough W F. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes[J]. Geological Society of London Special Publication, 1989, 42(1): 313-345.
[36] Xiong Longgen, Adam J, Green T H. Rutile Stability and Rutile/Melt HFSE Portioning During Melting of Hydrous Basalt: Implications for TTG Genesis[J]. Chenical Geology, 2005, 218: 339-359.
[37] 吴福元, 李献华, 杨进辉, 等.花岗岩成因研究的若干问题[J]. 岩石学报, 2007, 23(6): 1217-1238. Wu Fuyuan, Li Xianhua, Yang Jinhui,et al. Discussions on the Petrogenesis of Granites[J]. Acta Petrologica Sinica, 2007, 23(6): 1217-1238.
[38] Eby G N. The A-Type Granitiods: A Review of Their Occurrence and Chemical Characteristics and Speculations on Their Petrogenesis[J]. Lithos, 1990, 26(1): 115-134.
[39] Pitcher W S, Atherton M D, Cobbing E J, et al. Magmatism at a Plate Edge: The Peruvian Andes[M]. Glasgow: Blackie-Halsted Press, 1985:1-28.
[40] Chappell B W, White A J R. Two Contrasting Gra-nite Types[J]. Pacific Geology, 1974, 8:173-174.
[41] Loiselle M C,Wones D S. Characteristics and Origin of Anorogenic Granites[J] . Geological Societ y of America, 1979, 11(7): 468.
[42] White A J R. Souces of Granite Magmas[J]. Geol-ogical Society of America: Abstracts with Programs, 1979, 11: 539.
[43] 邱检生,王德滋,彭亚鸣,等. 浙江舟山桃花岛碱性花岗岩的岩石学和地球化学特征及成因探讨[J]. 南京大学学报,1996, 32(1): 80-89. Qiu Jiansheng, Wang Dezi, Peng Yaming, et al. Petrology, Geochemistry and Genesis of Taohuadao Alkli Granite in Zhoushan, Zhejiang Province[J]. Journal of Nanjing University(Nature Sciences), 1996, 32(1): 80-89.
[44] 王德滋,沈渭洲. 中国东南部花岗岩成因与地壳演化[J]. 地学前缘, 2003, 10(3): 209-220. Wang Dezi, Shen Weizhou. Genesis ofGranitoids and Crustalm Evolution in Southeast China[J]. Earth Science Frontiers, 2003, 10(3): 209-220.
[45] 苏玉平,唐红峰. A型花岗岩的微量元素地球化学[J]. 矿物岩石地球化学通报, 2005, 24(3): 245-251. Su Yuping, Tang Hongfeng. Trace Element Geochemistry of A-Type Granites[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2005, 24(3): 245-251.
[46] 周宇章,邢光福,杨祝良,等. 浙江诸暨新元古代后造山铝质A型花岗岩的厘定[J]. 地球学报,2006, 27(2): 107-113. Zhou Yuzhang, Xing Guangfu, Yang Zhuliang, et al.Recognition of Neoproterozoic Post-Orogenic Aluminous A-Type Granite in Zhuji, Zhejiang Province[J]. Acta Geoscientia Sinica,2006, 27(2): 107-113.
[47] 包志伟,赵振华. 佛冈铝质A型花岗岩的地球化学及其形成环境的初探[J].地质地球化学, 2003, 31(1):52-60. Bao Zhiwei,Zhao Zhenhua. Geochemistry and Tectonic Setting of the Fugang Aluminoua A-Type Granite, Guangdong Province, China:A Preliminary Study[J]. Geology-Geochemistry, 2003, 31(1):52-60.
[48] 刘昌实,刘小明,陈培荣,等. A型岩套的分类、判别标志和成因[J]. 高校地质学报, 2003, 9(4): 573-591. Liu Changshi, Liu Xiaoming, Chen Peirong, et al. Subdivision,Discrimination Criteria and Genesis for A Type Rock Suites[J]. Geological Journal of China Universities, 2003, 9(4): 573-591.
[49] Chappell B W,White A J R. Aluminium Saturation in I and S-Type Granites and the Characterization of Fractionated Haplogranites[J]. Lithos, 1999, 46(3): 535-551.
[50] Whalen J B,Currie K L,Chappell B W. A-Type Granites:Geochemical Characteristics Discrimination and Petrogenesis[J]. Contrib Mineral Petrol,1987,95(4):407-419.
[51] 陈行时, 张朋, 孙景贵, 等. 张广才岭英城子金矿区早古生代花岗岩的元素地球化学特征、岩石成因及构造意义[J]. 吉林大学学报(地球科学版), 2011, 41(2): 440-447. Chen Xingshi, Zhang Peng, Sun Jinggui,et al.Element Geochemistry and Genesis of Early Paleozoic Granite in Yingchengzi Gold-Field, Eastern Zhangguangcai Mountain and Its Tectonic Significance[J]. JournL of Jilin University(Earth Science Edition), 2011, 41(2): 440-447.
[52] 张金阳, 马昌前, 佘振兵, 等. 大别造山带北部铁佛寺早古生代同碰撞型花岗岩:地球化学和年代学证据[J]. 中国科学:D辑:地球科学,2007, 37(1): 1-9. Zhang Jinyang, Ma Changqian, She Zhenbing, et al. Syn-Collision Type Granite of Tiefosi in Early Paleozoic in the Northern of Dabie Orogenic Belt: Geochemistry and Chronology of Evidence[J]. Science in China:Series D:Earth Sciences, 2007, 37(1): 1-9.
[53] 徐克勤, 胡受奚, 孙明志, 等. 论花岗岩的成因系列:以华南中生代花岗岩为例[J]. 地质学报, 1983, 2: 107-118. Xu Keqin, Hu Shouxi,Sun Mingzhi, et al. On the Genetic Series of Granites as Exemplified by the Mesozoic Granites of South China[J]. Acta Geologica Sinica, 1983, 2: 107-118.
[54] Wu Fuyuan, Jahn B M, Simon A Wilde,et al. Highly Fractionated I-Type Granites in NE China(Ⅱ): Iisotopic Geochemistry and Implications for Crustal Growth in the Phanerozoic[J]. Lithos, 2003, 67: 191-204.
[55] Foley S,Peccerillo A. Potassic and Ultrapotassic Ma-gmas and Their Origin[J]. Lithos, 1992, 28: 181-185.
[56] Menzies M A, Fan W M, Zhang M. Palaeozoic and Cenozoic Lithoprobes and the Loss of > 120 km of Archaean Lithosphere, Sino-Korean Craton, China[C]//Prichard H M, Alabaster T, Harris N B W, et al. Magmatic Processes and Plate Tectonics. London:Geological Society Special Publication, 1993: 71-78.
[57] Pearce J A, Harris N B W,Tindle A G. Trace Element Discrimination Diagrams for the Ttectonic Interpretation of Granitic Rocks[J]. Journal of Petrology, 1984, 25(4): 956-983.
[58] 曾庆栋,褚少雄,刘江明,等. 西拉木伦成矿带中生代花岗岩浆活动与钼成矿作用[J]. 吉林大学学报(地球科学版),2011, 41(6): 1705-1725. Zeng Qingdong, Chu Shaoxiong, Liu Jiangming, et al. Mesozoic Granitic Magmatism and Molybdenum Ore-Forming Processes in the Xilamulun Metallogenic Belt[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(6): 1705-1725.
[59] Zhang Shuanhong, Zhao Yue, Song Biao, et al. Cont-rasting Late Carboniferous and Late Permian-Middle Triassic Intrusive Suites from the Northern Margin of the North China Craton: Geochronology, Petrogenesis and Tectonic Implications[J]. Geological Society of America Bulletin, 2009, 121: 181-200.
[60] 吴福元,孙德有. 中国东部中生代岩浆作用与岩石圈减薄[J]. 长春科技大学学报,1999, 29(4): 313-318. Wu Fuyuan, Sun Deyou. The MesozoicMagamatism and Lithospheric Thinning in Eastern China[J]. Journal of Changchun University of Science and Technology, 1999, 29(4): 313-318.
[61] 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.
[62] Zhai M G, Yang J H, Fan H R, et al. A Large-Scale Cluseter of Gold Deposits and Metallogenesis in the Eastern North China Craton[J]. International Geology Review, 2002, 44: 458-476.
[63] Zhang Shuanhong, Zhao Yue, Kroner A, et al. Early Permian Plutons from the Northern China Block: Constrants on Continental Are Evolution and Convergent Margin Magmatsim Related to the Central Asian Orogenic Belt[J]. International Journal of Earth Sciences, 2009, 98: 1441-1467.
[64] 赵越, 陈斌, 张拴宏, 等. 华北克拉通北缘及邻区前燕山期主要地质事件[J]. 中国地质, 2010, 37(4): 900-915. Zhao Yue, Chen Bin, Zhang Shuanhong, et al. Pre-Yanshanian Geological Events in the Northern Margin of the North China Craton and Its Adjacent Areas[J]. Geology in China, 2010, 37(4): 900-915.
[65] Sun Zhenjun,Sun Guosheng,Yu Henan,et al. The Geochronology, Geochemical Characteristics and Tectonic Significance of Intrusion in Jinchangliang Gold Deposit, Inner Mongolia[J]. Acta Geologica Sinica (English Edition), 2015, 89(6): 1947-1962.
[66] 宋维民,卞雄飞,邢德和,等. 辽宁北票地区江沟山岩体锆石U-Pb年代学和地球化学[J]. 地质与资源, 2010, 19(4): 339-345. Song Weimin, Bian Xiongfei,Xing Dehe, et al. U-Pb Zircon Geochronology and Geochemistry of Jianggoushan Intrusion in Beipiao Area, Liaoning, China[J]. Geology and Resources, 2010, 19(4): 339-345.
[67] 聂凤军,江思宏,张义,等. 中蒙边境中东段金属矿床成矿规律和找矿方向[M]. 北京:地质出版社,2007:1-574. Nie Fengjun,Jiang Sihong, Zhang Yi, et al. The Metal Deposit Metallogenic Regularities and Prospecting Direction in the Middle East Section of Border China and Mongulia[M].Beijing: Geological Publishing House, 2007:1-574.
[1] 张强, 丁清峰, 宋凯, 程龙. 东昆仑洪水河铁矿区狼牙山组千枚岩碎屑锆石U-Pb年龄、Hf同位素及其地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1085-1104.
[2] 郭春涛, 李如一, 陈树民. 塔里木盆地古城地区鹰山组白云岩稀土元素地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1121-1134.
[3] 崔亚川, 于介江, 杨万志, 张元厚, 崔策, 于介禄. 东天山觉罗塔格带黄山地区角闪辉长岩岩体的年代学、地球化学特征及岩石成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1105-1120.
[4] 赵希林, 姜杨, 邢光福, 于胜尧, 彭银彪, 黄文成, 王存智, 靳国栋. 陈蔡早古生代俯冲增生杂岩对华夏与扬子地块拼合过程的指示意义[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1135-1153.
[5] 王朝阳, 孟恩, 李壮, 李艳广, 靳梦琪. 吉东南新太古代晚期片麻岩类的时代、成因及其对早期地壳形成演化的制约[J]. 吉林大学学报(地球科学版), 2018, 48(3): 587-625.
[6] 高飞, 刘永江, 温泉波, 李伟民, 冯志强, 范文亮, 汤超. 内蒙古突泉—科尔沁右翼中旗地区中生代花岗岩锆石U-Pb年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(3): 769-783.
[7] 尹业长, 郝立波, 赵玉岩, 石厚礼, 田午, 张豫华, 陆继龙. 冀东高家店和蛇盘兔花岗岩体:年代学、地球化学及地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(2): 574-586.
[8] 齐天骄, 薛春纪, 许碧霞. 新疆昭苏布合塔铜(金)矿化区花岗质岩石锆石U-Pb年龄、地球化学特征及其成因[J]. 吉林大学学报(地球科学版), 2018, 48(1): 132-144.
[9] 孙凡婷, 刘晨, 邱殿明, 鲁倩, 贺云鹏, 张铭杰. 大兴安岭东坡小奎勒河中基性侵入岩成因及地球动力学意义:锆石U-Pb年代学、元素和Hf同位素地球化学证据[J]. 吉林大学学报(地球科学版), 2018, 48(1): 145-164.
[10] 孟恩, 王朝阳, 刘超辉, 施建荣, 李艳广. 辽东半岛东南部南辽河群变质火山岩的时代、成因及其对区域构造演化的制约[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1589-1619.
[11] 张超, 崔芳华, 张照录, 耿瑞, 宋明春. 鲁西金岭地区含矿闪长岩体成因:来自锆石U-Pb年代学和地球化学证据[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1732-1745.
[12] 施珂, 张达玉, 丁宁, 王德恩, 陈雪锋. 皖南逍遥岩体的年代学、地球化学特征及其成因分析[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1746-1762.
[13] 谭洪旗, 刘玉平. 滇东南猛洞岩群斜长角闪岩成因及其构造意义[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1763-1783.
[14] 高红梅, 兰永伟, 周莉, 孟丽岩. 温度作用下缺陷花岗岩热损伤:以甘肃北山缺陷花岗岩为例[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1795-1802.
[15] 陈治军, 任来义, 贺永红, 刘护创, 宋健. 银额盆地哈日凹陷银根组优质烃源岩地球化学特征及其形成环境[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1352-1364.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发