吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 673-689.doi: 10.13278/j.cnki.jjuese.20180271

• 地质与资源 • 上一篇    下一篇

吉林敦化松江河地区中生代似斑状花岗岩成因和形成环境:元素、Hf同位素和锆石U-Pb年代学证据

鲁倩1, 孙景贵1, 安久海2, 韩吉龙1, 褚小磊1   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林省有色金属地质勘查局, 长春 130012
  • 收稿日期:2018-10-22 出版日期:2019-06-03 发布日期:2019-06-03
  • 通讯作者: 孙景贵(1961-),男,教授,博士生导师,主要从事地球化学及热液矿床的研究与教学工作,E-mail:sunjinggui@jlu.edu.cn E-mail:sunjinggui@jlu.edu.cn
  • 作者简介:鲁倩(1994-),女,硕士研究生,主要从事岩石地球化学方面的研究,E-mail:1874462919@qq.com
  • 基金资助:
    国家科技部项目（2017YFC0601306）；中国地质调查局项目（DD2016005202）

Petrogenesis and Forming Environment of Mesozoic Porphyritic Granite in Songjianghe Region of Dunhua,Jilin Province: Evidences from Element Geochemistry,Hf Isotope and U-Pb

Lu Qian1, Sun Jinggui1, An Jiuhai2, Han Jilong1, Chu Xiaolei1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Jilin Nonferrous Metals Geological Exploration Bureau, Changchun 130012, China
  • Received:2018-10-22 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by the Program of Ministry Science and Technology of China(2017YFC0601306)and Project of China Geological Survey(DD2016005202)

PDF (PC)

301

摘要： 花岗岩是陆壳的重要组成部分，它是揭示地壳演化地球动力学过程的主要对象之一。为了揭示夹皮沟-海沟构造带的中生代地质演化，本文系统地开展了该带中段松江河地区花岗岩体内部产出的似斑状花岗岩的野外地质调查、岩相学、单颗粒锆石U-Pb同位素年代学、全岩元素、Hf同位素地球化学的研究。研究结果揭示：岩石呈粉红色、普遍发生较强的糜棱岩化作用，发育糜棱叶理构造；获得岩浆锆石的U-Pb同位素谐和年龄为217~169 Ma；加权平均年龄为（169.6±1.8） Ma（n=9，MSWD=1.3）；主量元素呈现高硅（71.18%~71.99%）、富碱（8.54%~8.93%）、贫镁（0.42%~0.52%）、贫钙（0.93%~1.38%）特征，并且A/NK>1.0，A/CNK<1.1；微量元素呈现低Rb、Zr和高Sr、Ba等质量分数，高Sr/Y和（La/Yb）N特征；稀土元素表现轻稀土元素富集、重稀土元素亏损和较弱Eu的正异常特征；获得锆石原位176Yb/177Hf值为0.010 517~0.050 159，176Lu/177Hf值为0.000 476~0.001 784，176Hf/177Hf为0.282 310~0.282 457，对应的锆石εHf（t）值为-12.7~-7.5，二阶段模式年龄为2 792~2 325 Ma。上述特征揭示，松江河地区中生代似斑状花岗岩属准中等分异、同碰撞向伸展转换的Ⅰ型花岗岩，原始岩浆起源于新太古代陆壳重熔作用，岩浆就位发生在中侏罗世早阶段；它记录了燕山期早侏罗世古太平洋板块向欧亚大陆之下俯冲的挤压陆壳活化产生岩浆，并于中侏罗世地壳伸展岩浆上升过程中经岩浆结晶分离作用而产生的中等分异岩浆结晶形成，成岩后于晚侏罗世遭受了韧脆性构造作用改造。

关键词: 元素地球化学, Hf同位素, 锆石U-Pb年代学, 岩石成因, 形成环境, 似斑状花岗岩

Abstract: As an important part of continental crust, granite is one of the main objects to reveal the dynamic process of crustal evolution. The research of geology,geochronology and geochemistry was carried out on the porphyritic granite in Songjianghe granite to reveal the Mesozoic geological evolution of Jiapigou-Haigou structural belt. The Songjianghe porphyritic granite is pink,and mylonitization and mylonite foliation structure are widely developed. Zircon U-Pb apparent ages range from 217 Ma to 169 Ma with a weighted mean age of (169.6±1.8)Ma (n=9,MSWD=1.3). The major element data show that the porphyritic granite is characterized by high SiO2(71.18%-71.99%),alkali (8.54%-8.93%),low MgO (0.42%-0.52%), CaO (0.93%-1.38%),A/NK greater than 1.0,and A/CNK less than 1.1. The trace element data reveal that the porphyritic granite is characterized by depletion of Rb and Zr,enrichment of Sr and Ba,and high Sr/Y and (La/Yb)N. The REEs are characterized by enrichment of LREE, loss of HREE, and weak negative Eu anomalies. Hf isotope data show that 176Yb/177Hf ranges from 0.010 517 to 0.050 159,176Lu/177Hf ranges from 0.000 476 to 0.001 784,176Hf/177Hf ranges from 0.282 310 to 0.282 457,and the εHf(t) value of zircon ranges from -12.7 to -7.5,and the two-stage Hf model ages range from 2 792 to 2 325 Ma. The above features indicate that the Songjianghe porphyritic granites belong to the medium differentiated Ⅰ-type granite,and its geodynamic background is related to the transition from syn-collision to extension. The primary magma was derived from a re-melting and emplacement of late Neoarchean crust in the early Middle Jurassic. The magmatism was associated with the continental crust activation caused by the subduction of the Paleo Pacific plate to the Eurasian plate in the Early Jurassic. The porphyritic granite was generated by medium differentiated magmatic crystallization during the magma rising in the Middle Jurassic crustal extension, and followed by the transformation of the Late Jurassic ductile-brittle tectonic action.

Key words: element geochemistry, Hf isotope, Zircon U-Pb geochronology, petrogenesis, forming environment, porphyritic granite

中图分类号: 

  • P581
[1] 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.
[2] 王涛,王晓霞,郑亚东,等.花岗岩构造研究及花岗岩构造动力学刍议[J].地质科学,2007,42(1):91-113. Wang Tao,Wang Xiaoxia,Zheng Yadong,et al. Studies on Structures of Granitic Plutons and Granitic Tectonic Dynam Ics[J].Chinese Journal of Geology,2007,42(1):91-113.
[3] 董申保.近代花岗岩研究的回顾[J].高校地质学报,1995,1(2):1-12. Dong Shenbao.A General Review on the Recent Studies of Granite[J].Geological Journal of Universities,1995,1(2):1-12.
[4] 韩振新,郝正平,侯敏.小兴安岭地区与加里东期花岗岩类有关的矿床成矿系列[J].矿床地质,1995,14(4):293-302. Han Zhenxin,Hao Zhengping,Hou Min.Metallogenic Series of Ore Deposits Related to Caledonian Granitoids in Xiao Hinganling Region[J].Mineral Deposits,1995,14(4):293-302.
[5] 洪大卫,王涛,童英.中国花岗岩概述[J].地质论评,2007,53(增刊):9-16. Hong Dawei,Wang Tao,Tong Ying. An Outline About Granitoids in China[J].Geological Review,2007,53(Sup.):9-16.
[6] 徐夕生,贺振宇. 花岗岩研究进展[J].矿物岩石地球化学通报,2012,31(3):205-209. Xu Xisheng,He Zhenyu.Progress in Granite Studies[J] Bulletin of Mineralogy,Petrology and Geochemistry,2012,31(3):205-209.
[7] 孙景贵,赵俊康,刘建明,等. 内蒙金厂沟梁金矿床流体包裹体的He-Ar同位素地球化学研究[J].矿床地质,2006,25(增刊1):193-196. Sun Jinggui,Zhao Junkang,Liu Jianming,et al. He-Ar Isotopic Geochemistry of Fluid Inclusions Research of Jinchanggouliang Gold Deposit,Inner Mongolia[J].Mineral Deposits,2006,25(Sup.1):193-196.
[8] 唐克东,王莹,何国琦,等. 中国东北及邻区大陆边缘构造[J].地质学报,1995,69(1):16-30. Tang Kedong,Wang Ying,He Guoqi,et al.Continental-Margin Structure of Northeast China and Its Adjacent Areas[J]. Acta Geologica Sinica,1995,69(1):16-30.
[9] 李锦轶.中国东北及邻区若干地质构造问题的新认识[J].地质论评,1998,44(4):339-347. Li Jinyi. Some New Ideas on Tectonics of NE China and Its Neighboring Areas[J].Geological Review,1998,44(4):339-347.
[10] 孙加鹏,张兴洲. 中新生代以来中国大陆的稳定地块[J].世界地质,1999,18(2):53-57. Sun Jiapeng,Zhang Xingzhou.The Stable Blocks in China Since Mesozoic and Cenozoic[J].Global Geology,1999,18(2):53-57.
[11] 吴福元,曹林. 东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13. Wu Fuyuan,Cao Lin.Some Important Problems of Geology in Northeastern Asia[J]. Global Geology,1999,18(2):1-13.
[12] 朱日祥,陈凌,吴福元,等.华北克拉通破坏的时间、范围与机制[J].中国科学:地球科学,2011,41(5):583-592. Zhu Rixiang,Chen Ling,Wu Fuyuan,et al.Timing,Scale and Meclimism of the Destruction of the North China Craton[J]. Science China:Earth Sciences,2011,41(5):583-592.
[13] 张艳斌,吴福元,李惠民,等.吉林黄泥岭花岗岩体的单颗粒锆石U-Pb年龄[J].岩石学报,2002,18(4):475-481. Zhang Yanbin,Wu Fuyuan,Li Huimin,et al. Single Grain Zircon U-Pb Ages of the Huangniling Granite in Jilin Province[J].Acta Petrologica Sinica,2002,18(4):475-481.
[14] Miao Laicheng,Qiu Yumin,Fan Weiming,et al. Geology,Geochronology,and Tectonic Setting of the Jiapigou Gold Deposits,Southern Jilin Province,China[J].Ore Geology Reviews,2005,26(1):137-165.
[15] Wu Fuyuan,Sun Deyou,Ge Wenchun,et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J].Journal of Asian Earth Sciences,2011,41(1):1-30.
[16] 黄志新. 吉林省夹皮沟金矿带构造-流体-成矿系统[D]. 北京:中国地质大学,2012. Huang Zhixin.Tectonics-Fluids-Mineralization System of Jiapigou Gold Belt in Jilin Province,China[D]. Beijing:China University of Geosciences,2012.
[17] Deng Jun,Yuan Wanming,Emmanuel John,et al. Geochronology and the Rmochronometry of the Jiapigou Gold Belt,Northeastern China:New Evidence for Multiple Episodes of Mineralization[J].Journal of Asian Earth Sciences,2014,89(3):10-27.
[18] 彭玉鲸,纪春华,辛玉莲,等.中俄朝毗邻地区古吉黑造山带岩石及年代记录[J].地质与资源,2002,11(2):65-75. Peng Yujing,Ji Chunhua,Xin Yulian,et al. Petrology and Geochronology of the Paleo-Jilin-Heilongjiang Orogenic Belt in the Adjecent Areas of China,Russia and Korea[J].Geology and Resources,2002,11(2):65-75.
[19] 王粉丽,王海鹏,鲁红峰.大兴安岭北上其地区晚石炭世花岗岩类LA-ICP-MS锆石U-Pb测年及地质意义[J].西北地质,2017,50(4):51-58. Wang Fenli,Wang Haipeng,Lu Hongfeng. LA-ICP-MS Zircon U-Pb Ages of Late Carboniferous Granites from Shangqi Area in Great Xing'an Range and Its Significance[J].Northwestern Geology,2017,50(4):51-58.
[20] 孙荣圭,Armstrong R L.辽东清原地区太古代岩石Rb-Sr年代[J].地球化学,1989,18(1):81-91. Sun Ronggui,Armstrong R L.Rb-Sr Geochronology of Archean Rocks in Qingyuan Area,Eastern Liaoning Province[J]. Geochimica,1989,18(1):81-91.
[21] 沈保丰,骆辉,李双保,等. 华北陆台太古宙绿岩带地质及成矿[M]. 北京:地质出版社,1994. Shen Baofeng,Luo Hui,Li Shuangbao,et al.Geology and Metallogenesis of Archean Green Belt in North China Platgorm[M].Beijing:Geological Publishing House,1994.
[22] 陈雷,孙景贵,陈行时,等.张广才岭东侧英城子金矿区花岗岩锆石U-Pb年龄及地质意义[J].地质学报,2009, 83(增刊1):1327-1334. Chen Lei,Sun Jinggui,Chen Xingshi,et al.Zircon LA-ICP-MS U-Pb Dating of Granite from the Yingchengzi Gold Deposit Area in the Eastern Zhangguangcailing Area and Its Geological Significance[J].Acta Geologica Sinica,2009, 83(Sup.1):1327-1334.
[23] 张旗,金惟俊,李承东,等.三论花岗岩按照Sr-Yb的分类:应用[J].岩石学报,2010,26(12):3431-3455. Zhang Qi,Jin Weijun,Li Chengdong,et al. On the Classification of Granitic Rocks Based on Whole-Rock Sr and Yb Concentrations Ⅲ:Practice[J].Acta Petrologica Sinica,2011,26(12)3431-3455.
[24] 罗镇宽,关康,苗来成. 吉林夹皮沟金矿带岩脉和蚀变绢云母定年及金矿成矿时代[J].现代地质,2002,16(1):19-25. Luo Zhenkuan,Guan Kang,Miao Laicheng. Dating of The Dykes and Altered Sericite in Jiapigou Gold Ore Belt,Jilin Province and Its Gold Ore Formation Age[J]. Geoscience,2002,16(1):19-25.
[25] 刘燊,胡瑞忠,冯彩霞,等. 吉林东部大蒲柴河adakites锆石U-Pb年龄、Hf同位素特征及其意义[J].岩石学报,2009,25(12):3153-3164. Liu Shen,Hu Ruizhong,Feng Caixia,et al. Zircon U-Pb Age,Hf Isotopic Compositions of Dapuchaihe Adakites in Eastern Jilin Province and Their Significances[J].Acta Petrologica Sinica,2009,25(12):3153-3164.
[26] 李亮. 吉林省夹皮沟-海沟金成矿带金矿床成矿流体特征与深部成矿潜力评价[D]. 长春:吉林大学,2016. Li Liang.Research on Ore-Forming Fluids of Gold Deposits in Jiapigou-Haigou Gold Belt,Jilin Province and Deep-Seated Metallogenic Assessment[D].Changchun:Jilin University,2016.
[27] Li Liang,Sun Jinggui,Men Lanjing,et al. Origin and Evolution of the Ore-Forming Fluids of the Erdaogou and Xiaobeigou Gold Deposits,Jiapigou Gold Province,NE China[J].Journal of Asian Earth Sciences,2016,129:170-190.
[28] 王淑娟,姜亚洁,梅国良,等. 吉林省桦甸市老牛沟铁矿床地质特征[J].吉林地质,2010,29(3):50-55. Wang Shujuan,Jiang Yajie,Mei Guoliang,et al. Geological Features of the Laoniugou Iron Deposit,Huadian City of Jilin Province[J]. Jilin Geology,2010,29(3):50-55.
[29] 史致元,武殿军,孔清明. 桦甸市双山头铁矿床地质特征及找矿标志[J].吉林地质,2009,28(3):43-46. Shi Zhiyuan,Wu Dianjun,Kong Qingming. Geological Characteristics and Prospecting Criteria of the Shuangshantou Iron Deposit in Huadian City[J].Jilin Geology,2009,28(3):43-46.
[30] Wu Fuyuan,Yang Yueheng,Xie Liewen,et al. Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology[J].Chemical Geology,2006,234(1):105-126.
[31] Griffin W L,Wang Xiang,Jackson S E,et al. Zircon Chemistry and Magma Mixing,SE China:In-Situ Analysis of Hf Isotopes,Tonglu and Pingtan Igneous Complexes[J]. Lithos,2002,61(3):237-269.
[32] Woodhead J,Hergt J,Shelley M,et al. Zircon Hf-Isotope Analysis with an Excimer Laser,Depth Profiling,Ablation of Complex Geometries,and Concomitant Age Estimation[J].Chemical Geology,2004,209(1):121-135.
[33] Bievre P D,TaylorP D P.Table of the Isotopic Compositions of the Elements[J].International Journal of Mass Spectrometry & Ion Processes,1993,123(2):149-166.
[34] Wang Richu,Liu Chunlei,Jin Zhanpeng. Determination of Isothermal Section of Ni-Re-Hf Ternary System at 1173 K[J].Journal of Central South University,2002,9(2):77-80.
[35] Collins W J,Beams S D,White A J R,et al.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia[J].Contributions to Mineralogy & Petrology,1982,80(2):189-200.
[36] Irvine T N,Bargee W R A.A Guide to the Chemical Classifieation of the Common Volcanic Meks[J].Canadian Journal of Earth Seienees,1971,8:523-548.
[37] Sun R,Armstrong K L. Rb-Sr Geochronology of Archean Rocks in Qingyuan Area[J]. Geochimica,1989,18(1),81-91.
[38] 李俊建,沈保丰,李双保,等. 辽北-吉南地区太古宙花岗岩-绿岩带地质地球化学[J].地球化学,1996,25(5):458-467. Li Junjian,Shen Baofeng,Li Shuangbao,et al. Geology and Geochemistry of Archean Granite-Greenstnoe Belts in Northern Liaoning Province and Southern Jilin Province[J].Geochimica,1996,25(5):458-467.
[39] 李俊建,沈保丰. 辽北-吉南早前寒武纪大陆壳的地质特征和演化[J].地质通报,1998,17(1):30-38. Li Junjian,Shen Baofeng.Geological Feature and Evolution of the Early Precambrian Continental Crust in Northern Liaoning Province and Southern Jilin Province[J].Regional Geology of China,1998,17(1):30-38.
[40] Chappell B W,White A J R.Two Contarsting Granite Types[J]. Pacific GeoSource,1974,8:173-174.
[41] Ishihara S.The Magnetite-Series and Ilmenite-Series Granitic Rocks[J].Mining Geology,1977,27:293-305.
[42] Loisella M C,Wones D R. Characteristics and Origin of Anorogenie Granites[C]//GSA Abstracts. Boulder:Geological of Society of America,1979:468.
[43] Castro,王宇红. H型(混染)花岗岩类:花岗岩类型分类与命名的修改意见[J].华南地质与矿产,1992,7(4):1-8. Castro,Wang Yuhong. H Type (Mixed Dyed) Granitoids:Revision of Classification and Nomenclature of Granite Types[J].Geology and Mineral Resources of South China,1992,7(4):1-8.
[44] Whalen J B,Cyrrie K L,Chapple B W.A-Type Granites:Geochemical Characteristics Discrim Ination and Pertogenesis[J]. Contrib Mineral Petrol,1987,95:407-419.
[45] Taylor S R,McLennan S M.The Continental Crust:Its Composition and Evolution[J].Geological Magazine,1985,122(6):673-674.
[46] Taylor S R,Mclennan S M. The Geochemical Evolution of the Continental Crust[J].Reviews of Geophysics,1995,33(2):241-265.
[47] Mcdonough W F.Compositional Model for the Earth's Core[J].Treatise on Geochemistry,2003,2:547-568.
[48] 王朝阳,孟恩,李壮,等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):3-41. Wang Chaoyang,Meng En,Li Zhuang,et al.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):3-41.
[49] Wu Fuyuan.The Hulan Group:Its Role in the Evolution of the Central Asian Orogenic Belt of NE China[J].Journal of Asian Earth Sciences,2007,30(3):542-556.
[50] Chen Bin,Jahn B M,Suzuki K. Petrological and Nd-Sr-Os Isotopic Constraints on the Origin of High-Mg Adakitic Rocks from the North China Craton:Tectonic Implications[J].Geology,2013,41(1):91-94.
[51] 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.
[52] 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.
[53] 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 and Its Constraint on the Timing of Collision Between Siberian and Sino-Korean Paleo-Plates[J]. Acta Petrologica Sinica,2007,23(3):565-582.
[54] Wu Fuyuan,Sun Deyou,Li Huimin,et al. A-Type Granites in Northeastern China:Age and Geochemical Constraints on Their Petrogenesis[J].Chemical Geology,2002,187(1):143-173.
[55] 葛文春,吴福元,周长勇,等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J].岩石学报,2005,21(3):749-762. Ge Wenchun,Wu Fuyuan,Zhou Changyong,et al. Zircon U-Pb Ages and Its Significance of the Mesozoic Granites in the Wulanhaote Region,Central Da Hinggan Mountain[J].Acta Petrologica Sinica,2005,21(3):749-762.
[56] 孙德有,吴福元,高山.小兴安岭东部清水岩体的锆石激光探针U-Pb年龄测定[J].地球学报,2004,25(2):213-218. Sun Deyou,Wu Fuyuan,Gao Shan. LA-ICP-MS Zircon U-Pb Age of the Qingshui Pluton in the East Xiao Hinggan Mountains[J].Acta Eoscientica Sinica,2004,25(2):213-218.
[57] 冯光英,刘燊,冯彩霞,等.吉林红旗岭超基性岩体的锆石U-Pb年龄、Sr-Nd-Hf同位素特征及岩石成因[J].岩石学报,2011,27(6):1594-1606. Feng Guangying,Liu Shen,Feng Caixia,et al. Zircon U-Pb Ages,Sr-Nd-Hf Isotope Geochemistry and the Petrogenesis of the Ultramafic Pluton in Hongqiling,Jilin Province[J].Acta Petrologica Sinica,2011,27(6):1594-1606.
[58] Wu Fuyuan,Simon Wilde,Sun Deyou,et al.Geochronology and Petrogenesis of the Post-Orogenic Cu-Ni Sulfide-Bearing Mafic-Ultaamafic Complexes in Jilin Province,NE China[J].Journal of Asian Sciences,2004,23:781-797.
[59] 李承东,郑建民,张英利,等. 化德群的重新厘定及其大地构造意义[J].中国地质,2005,32(3):353-362. Li Chengdong,Zheng Jianmin,Zhang Yingli,et al.Redefinition of the Huade Group and Its Tectonic Significance[J].Geology in China,2005,32(3):353-362.
[60] 孙景贵,张勇,邢树文,等. 兴蒙造山带东缘内生钼矿床的成因类型、成矿年代及成矿动力学背景[J].岩石学报,2012,28(4):1317-1332. Sun Jinggui,Zhang Yong,Xing Shuwen,et al. Genetic Types,Ore-Forming Age and Geodynamic Setting of Endogenic Molybdenum Deposits in the Eastern Edge of Xing-Meng Orogenic Belt[J].Acta Petrologica Sinica,2012,28(4),1317-1332.
[61] 许文良,王枫,裴福萍,等. 中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353. Xu Wenliang,Wang Feng,Pei Fuping,et al. Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J].Acta Petrologica Sinica,2013,29(2):339-353.
[62] 王成辉,松权衡,王登红,等. 吉林大黑山超大型钼矿辉钼矿铼-锇同位素定年及其质意义[J].岩矿测试,2009,28(3):269-273. Wang Chenghui,Song Quanheng,Wang Denghong,et al. Re-Os Isotopic Dating of Molibdenite from the Daheishan Molybdenum Deposit of Jilin Province and Its Geological Significance[J].Rock and Mineral Analysis,2009,28(3):269-273.
[63] 李立兴,松权衡,王登红,等. 吉林福安堡钼矿中辉钼矿铼-锇同位素定年及成矿作用探讨[J].岩矿测试,2009,28(3):283-287. Li Lixing,Song Quanheng,Wang Denghong,et al.Re-Os Isotopic Dating Molybdenite from the Fu'anpu Molybdenum Deposit of Jilin Province and Discussion on Its Metallogenesis[J].Rock and Mineral Analysis,2009,28(3):283-287.
[64] Martina H,Smithies R H,Rapp R,et al. An Overview of Adakite,Tonalite Trondhjemite Granodiorite (TTG),and Sanukitoid:Relationships and Some Implications for Crustal Evolution[J].Lithos,2005,79:1-24.
[65] Pearce J A,Harris N B W,Tindle A G. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks[J]. Jour Petrol,1984,25(4):956-983.
[66] 李承东,张福勤,苗来成,等.吉林色洛河群的重新认识[J].吉林大学学报(地球科学版),2007,37(5):841-847. Li Chengdong,Zhang Fuqin,Miao Laicheng,et al.Reconsideration of the Seluohe Group in Seluohe Area,Jilin Province[J].Journal of Jilin University (Earth Science Edition),2007,37(5):841-847.
[1] 王春光, 董晓杰, 徐仲元, 任云伟, 王文龙, 陈煜嵩. 内蒙古红山子地区新太古代变质侵入岩年代学及地球化学特征[J]. 吉林大学学报(地球科学版), 2019, 49(3): 709-726.
[2] 张超, 吴新伟, 张渝金, 郭威, 权京玉. 龙江盆地中生代火山岩锆石U-Pb年代学及其对基底性质的制约[J]. 吉林大学学报(地球科学版), 2019, 49(2): 460-476.
[3] 殷征欣, 王海峰, 韩金生, 吕修亚, 沈泽中, 陈静, 贺惠忠, 谢安远, 关瑶, 董超. 南海边缘海多金属结核与大洋多金属结核对比[J]. 吉林大学学报(地球科学版), 2019, 49(1): 261-277.
[4] 尹志刚, 李海娜, 张海, 郝科, 庞学昌, 宫兆民, 李敏, 张圣听. 大兴安岭加格达奇东北部花岗岩类形成时代、地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1741-1755.
[5] 张朋, 寇林林, 赵岩, 毕中伟. 辽宁树基沟铜锌矿床黑云斜长角闪片麻岩锆石U-Pb年龄、Hf同位素组成及其地质意义[J]. 吉林大学学报(地球科学版), 2018, 48(5): 1365-1377.
[6] 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.
[7] 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.
[8] 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.
[9] 乔健, 栾金鹏, 许文良, 王志伟, 赵硕, 郭鹏. 佳木斯地块北部早古生代沉积建造的时代与物源:来自岩浆和碎屑锆石U-Pb年龄及Hf同位素的制约[J]. 吉林大学学报(地球科学版), 2018, 48(1): 118-131.
[10] 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.
[11] 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.
[12] 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.
[13] 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.
[14] 杨凤超, 宋运红, 赵玉岩. 辽宁盘岭矿集区花岗岩锆石SHRIMP U-Pb年龄、Hf同位素组成及地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1429-1441.
[15] 许中杰, 蓝艺植, 程日辉, 李双林. 句容地区下奥陶统仑山组海平面变化的碳酸盐岩地球化学记录[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1458-1470.
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