吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (3): 769-783.doi: 10.13278/j.cnki.jjuese.20170194

• 地质与资源 • 上一篇    下一篇

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

高飞1,2, 刘永江1,2, 温泉波1, 李伟民1, 冯志强3, 范文亮4, 汤超5   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 东北亚矿产资源评价国土资源部重点实验室, 长春 130061;
    3. 太原理工大学矿业工程学院, 太原 030024;
    4. 长春黄金研究院, 长春 130012;
    5. 中国地质调查局天津地质调查中心非化石能源矿产实验室, 天津 300170
  • 收稿日期:2017-09-17 出版日期:2018-05-26 发布日期:2018-05-26
  • 通讯作者: 刘永江(1964-),男,教授,博士生导师,主要从事大地构造学、构造年代学教学与研究,E-mail:yongjiang@jlu.edu.cn E-mail:yongjiang@jlu.edu.cn
  • 作者简介:高飞(1992-),男,硕士研究生,主要从事构造地质学方面的研究,E-mail:geophy0917@163.com
  • 基金资助:
    国家自然科学基金重点项目(41230206,41102140,41602235);中国地质调查局天津地质调查中心项目(DD20160128-04)

Zircon U-Pb Ages and Its Geological Implication of Mesozoic Granites in Tuquan-Keerqin Youyizhongqi Region

Gao Fei1,2, Liu Yongjiang1,2, Wen Quanbo1, Li Weimin1, Feng Zhiqiang3, Fan Wenliang4, Tang Chao5   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources of China, Changchun 130061, China;
    3. College of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, China;
    4. Changchun Gold Research Institute, Changchun 130012, China;
    5. Laboratory of Non-fossil Energy Minerals, Tianjin Center of China Geological Survey, Tianjin 300170, China
  • Received:2017-09-17 Online:2018-05-26 Published:2018-05-26
  • Supported by:
    Supported by National Natural Science Foundation of China(41230206,41102140,41602235) and Project Tianjin Center of China Geological Survey(DD20160128-04)

摘要: 内蒙古突泉—科尔沁右翼中旗地区位于大兴安岭中南段,中生代岩浆活动较为频繁,岩浆作用形成的岩石类型主要包括花岗闪长岩、正长花岗岩、二长花岗岩和花岗斑岩等。鉴于目前研究区地质资料缺乏对整个突泉—科右中旗地区中生代花岗岩较为完善的研究和论述,笔者旨在对全区范围内的中生代花岗岩进行LA-ICP-MS锆石U-Pb年龄测定,同时在总结前人资料的基础上划分该地区不同的中生代岩浆作用期次,进而讨论本区不同花岗岩所代表的地质意义。花岗岩锆石U-Pb年龄测试结果表明,孟恩陶勒盖花岗闪长岩的形成时代为(241.2±2.8) Ma,杜尔基镇南部正长花岗岩的形成时代为(148.2±1.0) Ma,宝格吐岩体的花岗闪长岩的形成时代为(226.0±1.1) Ma,马家屯花岗斑岩的形成时代为(124.6±1.1) Ma,这与广泛分布于本区中生代火山岩的形成时代较为一致。结合前人研究成果以及邻区的地质资料,认为本区岩浆活动可以划分为中—晚三叠世、晚侏罗世和早白垩世;中—晚三叠世花岗岩可能属于古亚洲洋闭合造山后岩石圈伸展作用的产物,而晚侏罗世花岗岩的形成可能与中侏罗世蒙古—鄂霍茨克洋闭合后岩石圈伸展作用有关,早白垩世花岗岩可能反映了板内拉张的构造背景。

关键词: 大兴安岭, 突泉-科尔沁右翼中旗地区, 中生代, 花岗岩, 锆石U-Pb测年

Abstract: Tuquan-Keerqin Youyizhongqi of Inner Mongolia is located in the central and southern Da Hinggan Range, where the Mesozoic magmatic activity was frequent. The rocks are mainly composed of granodiorite, syenite, monzonitic granite, and granite porphyry etc. We studied the Mesozoic granites in the whole area to obtain the related geological data,tested the LA-ICP-MS zircon U-Pb age,divided the different Mesozoic magmatism periods on the basis of the predecessors' data,and then discussed the geological significance of the different granites in this area. Several samples of the three magmatic intrusive rocks from this region were dated by the LA-ICP-MS technique. The result indicates that the granodiorite of Mengentaolegai pluton was emplaced at (241.2±2.8) Ma, the syenite in the southern Duerji was emplaced at (148.2±1.0) Ma, the monzonitic granite of Baogetu pluton was emplaced at (226.0±1.1) Ma, and the granite porphyry of the Majiatun pluton was emplaced at (124.6±1.1) Ma, corresponding to the ages of the volcanic rocks respectively. Combining with the previous and adjacent geological data, we divided the magmatic activity into three periods:Middle-Late Triassic, Late Jurassic, and Early Cretaceous. We conclude that the Middle-Late Triassic granites may be the product of the post-orogenic lithospheric extension of the Paleo-Asian Ocean closure, and the formation of the Late Jurassic granites may be related to the Mongol-Okhotsk Ocean closure; while the Early Cretaceous granites might reflect the extensional tectonic setting.

Key words: Da Hinggan Range, Tuquan-Keerqin Youyizhongqi area, Mesozoic, granite, zircon U-Pb age

中图分类号: 

  • P588.1
[1] 宋维民,巩恩普,刘世伟,等.内蒙古科尔沁右翼中旗孟恩陶勒盖岩体年代学研究[J].东北大学学报(自然科学版),2014,35(6):898-902. Song Weimin, Gong Enpu, Liu Shiwei, et a1.Study on the Geochronology of Meng'entaolegai Pluton in Horqin Right Wing Middle Banner, Inner Mongolia[J].Journal of Northeastern University (Natural Science), 2014, 35(6):898-902.
[2] 宋维民,庞雪娇,付俊彧,等.内蒙古科尔沁右翼中旗碱长花岗岩锆石U-Pb年代学、岩石地球化学动力学意义[J].吉林大学学报(地球科学版),2015,45(3):847-859. Song Weimin, Pang Xuejiao, Fu Junyu, et al. Zircon U-Pb Geochronology, Geochemistry and Dynamics of the Alkali Feldspar Granite in Horqin Right Wing Middle Banner of Inner Mongolia, with Implications for the Geodynamic Setting[J].Journal of Jilin University(Earth Science Edition), 2015, 45(3):847-859.
[3] 张明,付俊彧,肖剑伟,等.内蒙古孟恩陶勒盖岩体的成岩时代:LA-ICP-MS锆石U-Pb同位素年代学[J].地质与资源,2013,22(1):36-40. Zhang Ming, Fu Junyu, Xiao Jianwei, et a1. Petrogenie Age of Meng'entaolegai Intrusive Body in Inner Mongolia:LA-ICP-MS Zircon U-Pb Isotopic Geochronology[J].Geology and Resources, 2013, 22(1):36-40.
[4] 陈丽丽,陈志国.内蒙古兴安盟杜尔基地区花岗岩岩石学及锆石U-Pb年龄[J].中国地质,2015,42(4):891-908. Chen Lili, Chen Zhiguo.Petrology and Zircon Chronology of the Dorolj Granite in Hinggan League, Inner Mongolia[J].Geology in China, 2015, 42(4):891-908.
[5] 宋维民, 陶楠, 庞雪娇,等.内蒙古科尔沁右翼中旗敖兰三队侵入体年龄及地球化学特征[J].地质通报,2016,35(6):932-942. Song Weimin, Tao Nan, Pang Xuejiao, et al. Geochronology and Geochemistry of the Aolansandui Pluton in Horqin Right Wing Middle Banner of Inner Mongolia[J].Geological Bulletin of China, 2016, 35(6):932-942.
[6] 刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951. Liu Yongjiang, Zhang Xingzhou, Jin Wei, et al. Late Paleozoic Tectonic Evolution in Northeast China[J].Geology in China, 2010, 37(4):943-951.
[7] 吉林省地质矿产局.吉林省区域地质志[M].北京:地质出版社,1988:365-367. Jilin Bureau of Geology and Mineral Resources.Regional Geology of Jilin Province[M].Beijing:Geological Publishing House,1988:365-367.
[8] 内蒙古地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1991:1-725. Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Region.Regional Geology of Inner Mongolia Autonomous Region[M].Beijing:Geological Publishing House,1991:1-725.
[9] 陈树旺,张海华,郑月娟,等.内蒙古科右中旗-突泉地区晚二叠世林西组碎屑岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2015,34(10):1869-1877. Chen Shuwang, Zhang Haihua, Zheng Yuejuan, et al. Detrital Zircon LA-ICP-MS U-Pb Age of the Late Permian Linxi Formation in Horqin Right Wing Middle Banner-Tuquan Area of Inner Mongolia and Its Geological Significance[J].Geological Bulletin of China, 2015, 34(10):1869-1877.
[10] 丁秋红,陈树旺,郑月娟,等.大兴安岭地区突泉盆地侏罗系充填序列及暗色泥岩发育特征[J].地质与资源,2010,19(3):203-207. Ding Qiuhong, Chen Shuwang, Zheng Yuejuan, et al. The Development of Melamustone and the Jurussic Filling Sequence in Tuquan Basin,Daxing'anling Region[J]. Geology and Resources, 2010, 19(3):203-207.
[11] 张海华,郑月娟,陈树旺,等.内蒙古科尔沁右翼中旗三叠纪花岗质岩锆石U-Pb年龄、地球化学特征及其地质意义[J].吉林大学学报(地球科学版),2015,45(2):417-428. Zhang Haihua,Zheng Yuejuan,Chen Shuwang,et al. Zircon U-Pb Age,Geochemical Characteristics and Geological Significance of the Triassic Granite in Keerqinyouyizhongqi,Inner Mongolia[J].Journal of Jilin University(Earth Science Edition), 2015,45(2):417-428.
[12] 江思宏,聂凤军,刘翼飞, 等.内蒙古孟恩陶勒盖银多金属矿床及其附近侵入岩的年代学[J].吉林大学学报(地球科学版),2011,41(6):1755-1769. Jiang Sihong, Nie Fengjun, Liu Yifei, et al. Geochronology of Intrusive Rocks Occurring in and Around the Meng'entaolegai Agpolymetallic Deposit, Inner Mongolia[J].Journal of Jilin University (Earth Science Edition), 2011, 41(6):1755-1769.
[13] 丛立民,李国志. 内蒙古兴安盟杜尔基岩体特征研究[J].甘肃地质,2008,17(3):74-79. Cong Limin, Li Guozhi. Study on Characteristics of Duerji Intrusive in Xing'anmeng Area of Inner Mongolia[J]. Gansu Geology, 2008, 17(3):74-79.
[14] Yuan H, Gao S, Liu X, et al. Accurate U-Pb Age and Trace Element Determinations of Zirconby Laser Ablationinductively Coupled Plasmamass Spectrometry[J].Geostandards and Geoanalytical Research, 2004, 28(3):353-370.
[15] Andersen T. Correction of Common Lead in U-Pb Analyses That Do Not Report 204Pb[J].Chemical Geology, 2002, 192(1):59-79.
[16] Diwu C R, Sun Y, Yuan H L, et al. U-Pb Ages and Hf Isotopes for Detrital Zircons from Quartzite in the Paleoproterozoic Songshan Group on the Southwestern Margin of the North China Craton[J].Chinese Science Bulletin, 2008, 53(18):2828-2839.
[17] Ludwig K R.Mathematical-Statistical Treatment of Data and Errors for 230Th/U Geochronology[J].Reviews in Mineralogy and Geochemistry, 2003, 52(1):631-656.
[18] 王忠禹,孙景贵,白令安,等.内蒙古莲花山铜矿区花岗闪长斑岩LA-ICP-MS锆石U-Pb年龄[J].地质通报,2014,33(9):1320-1325. Wang Zhongyu, Sun Jinggui, Bai Ling'an, et al. LA-ICP-MS Zircon U-Pb Dating of Granodiorite Porphyry in the Lianhuashan Copper Deposit of Inner Mongolia and Its Geological Implications[J].Geological Bulletin of China, 2014, 33(9):1320-1325.
[19] 周振华,武新丽,欧阳荷根.内蒙古莲花山铜银矿斜长花岗斑岩LA-MC-ICP-MS锆石U-Pb测年、Hf同位素研究及其地质意义[J].中国地质,2012,39(6):1472-1485. Zhou Zhenhua, Wu Xinli, Ou'yang Hegen. LA-ICP-MS Zircon U-Pb Dating, Hf Isotope Study of the Plagioclase Granite Porphyry from the Lianhuashan Cu-Ag Deposit in Inner Mogolia and Its Geological Significance[J]. Geology in China, 2012, 39(6):1472-1485.
[20] 古阿雷,孙景贵,白令安,等.大兴安岭中东部闹牛山浅成热液脉型铜矿床成岩成矿机理研究:来自地球化学及年代学制约[J].吉林大学学报(地球科学版),2015,45(增刊1):1548. Gu Alei, Sun Jinggui, Bai Ling'an, et al. Study on Metallogenic Mechanism about Epithermal Copper Deposits of Naoniu Mountain in the Central and East of the Great Xing'an Range:Which from the Constraints Related to Geochemistry and Chronology[J].Journal of Jilin University(Earth Science Edition), 2015, 45(Sup.1):1548.
[21] 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 a1.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.
[22] 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.Zircon U-Pb Age of the Qingshui Pluton in the East Xiaoxing'an Mountains[J].Acta Geoscientia Sinica, 2004, 25(2):213-218.
[23] 杨奇荻,郭磊,王涛,等.大兴安岭中南段甘珠尔庙地区晚中生代两期花岗岩的时代、成因、物源及其构造背景[J].岩石学报,2014,30(7):1961-1981. Yang Qidi, Guo Lei, Wang Tao, et al. Geochronology, Origin, Ources and Tectonic Settings of Late Mesozoic Two-Stage Granites in the Ganzhuermiao Region, Central and Southern Da Hinggan Range, NE China[J].Acta Petrologica Sinica, 2014, 30(7):1961-1981.
[24] 陈会军,张彦龙,汪清海,等. 大兴安岭中段早白垩世花岗质岩石锆石U-Pb年龄及地球化学特征[J].地质与资源,2014,24(5):1671-1647. Chen Huijun, Zhang Yanlong, Wang Qinghai, et al. Zircon U-Pb Dating and Geochemistry of the Early Cretaceous Granitic Rocks in the Middle Section of Daxing'anling Mountains[J]. Geology and Resources, 2014, 24(5):1671-1647.
[25] 赵辉,李舢,王涛,等.大兴安岭南段黄岗梁地区早白垩世岩浆作用的时代、成因及其构造意义[J].地质通报,2015,34(12):2203-2218. Zhao Hui, Li Shan, Wang Tao, et al. Age, Petrogenesis and Tectonic Implications of the Early Cretaceous Magmatism in the Huanggangliang Area, Southern Da Hinggan Mountains[J].Geological Bulletin of China, 2015, 34(12):2203-2218.
[26] 王忠,朱洪森. 大兴安岭中南段中生代火山岩特征及演化[J].中国区域地质,1999,18(4):351-358. Wang Zhong, Zhu Hongsen.Temporal and Spatial Evolution of the Mesozoic Volcanism in Mid-Southern Daxing'anling Mountain[J].Regional Geology of China, 1999, 18(4):351-358.
[27] 孙德有,吴福元,林强,等.张广才岭燕山早期白石山岩体成因与壳幔相互作用[J].岩石学报,2001,17(2):227-235. Sun Deyou, Wu Fuyuan, Lin Qiang, et al. Petrogenesis of the Crust-Mantle Interaction of Early Yanshanian Baishishan Pluton in Zhangguangcai Range[J].Acta Petrologica Sinica, 2001, 17(2):227-235.
[28] 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. Singie Grain Zircon U-Pb Ages of the Huangniling Granite in Jilin Province[J].Acta Petrologica Sinica, 2002, 18(4):475-481.
[29] 张艳斌,吴福元,翟明国,等.和龙地块的构造属性与华北地台北缘东段边界[J].中国科学:D辑:地球科学,2004,34(9):795-806. Zhang Yanbin, Wu Fuyuan, Zhai Mingguo, et al. The Tectonic Attributes of the Helong Block and the Eastern Borderline of the North Margin of North China Craton[J].Science in China:Series D:Earth Sciences, 2004, 34(9):795-806.
[30] 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 Xiramuron-Changchun-Yanji Plate Suture Zone:Evidence from the Dayushan Granitic Pluton of Jilin[J].Journal of Jilin University (Earth Science Edition), 2004, 34(2):174-181.
[31] Wu Fuyuan, Jahn B M, Wilder S A, et al. Highly Fractionated I-Type Granites in NE China:Geochronology and Petrogenesis[J]. Lithos, 2003, 66(3):241-273.
[32] Dmitry V M, Valery A V, Alexey Y K, et al. Late Mesozoic Tectonics of Central Asia Based on Paleomagnetic Evidence[J].Gondwana Research, 2010, 18(2), 400-419.
[33] Donskaya T V, Gladkochub D P, Mazukabzov A M, et al. Late Paleozoic-Mesozoic Subduction-Related Magamatism at the Southern Margin of the Siberian Contient and the 150 Million Year History of the Mongol-Okhostsk Ocean[J].Journal of Asian Earth Sciences, 2013, 62:79-97.
[34] 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 Palco-Plates[J].Acta Petrologica Sinica, 2007, 23(3):565-582.
[35] 高福红,许文良,杨德彬,等.松辽盆地南部基底花岗质岩石锆石LA-ICP-MS U-Pb定年:对盆地基底形成时代的制约[J].中国科学:D辑,2007,37(3):331-335. Gao Fuhong, Xu Wenliang, Yang Debin, et al. Zircon Dating on the Granitoid Rocks from the Basement of the Southern Songliao Basin:Constrants on the Forming Time of the Basement[J].Science in China:Series D, 2007, 37(3):331-335.
[36] Xu W L, Pei F P, Wang F, et al. Spatial-Temporal Relationships of Mesozoic Volcanic Rocks in NE China:Constraints on Tectonic Overprinting and Transformations Between Multiple Tectonic Regimes[J].Journal of Asian Earth Sciences, 2013, 74:167-193.
[37] Wu F Y, Sun D Y, Li H M, et al. A-Type Granites in Northeastern China:Age and Geochemistry Constrains on Their Petrogenesis[J].Chemical Geology, 2002, 187(1):143-173.
[38] Jahn B M, Litvinovsky B A, Zanvilevich A N, et al. Peralkaline Granitoid Magmatism in the Mongolian-Transbaikalian Belt:Evolution, Petrogenesis and Tectonic Significance[J]. Lithos, 2009, 113(3):521-539.
[39] 林强,葛文春,吴福元,等.大兴安岭中生代花岗岩类的地球化学[J].岩石学报,2004,20(3):403-412. Lin Qiang, Ge Wenchun, Wu Fuyuan, et al. Geochemistry of Mesozoic Granites in Da Hinggan Ling Ranges[J].Acta Petrologica Sinica, 2004, 20(3):403-412.
[40] Jahn B M, Wu F Y, Capdevila R, et al. Highly Evolved Juvenile Granites with Tetrad REE Patterns:The Wodube and Baerzhe Granites from the Great Xing'an Mountains in NE China[J]. Lithos, 2001, 59(4):171-198.
[41] Gao S, Rudnick R L, Carlson R W, et al. Re-Os Evidence for Replacement of Ancient Mantle Lithosphere Beneath the North China Craton[J].Earth and Planetary Science Letters, 2002, 198(3):307-322.
[42] Zhu R X, Chen L, Wu F Y, et al. Timing, Scale and Mechanism of the Destruction of the North China Craton[J]. Science in China:Series D, 2011, 54(6):789-797.
[43] Mao J, Wang Y, Zhang Z, et al. Geodynamic Settings of Mesozoic Large-Scale Mineralization in North China and Adjacent Areas[J]. Science in China:Series D:Earth Sciences, 2003, 46(8):838-851.
[44] 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.
[45] Dong Y, Ge W C, Yang H, et al. Geochronology and Geochemistry of Early Cretaceous Volcanic Rocks from the Baiyingaolao Formation in the Central Great Xing'an Range, NE China, and Its Tectonic Implications[J]. Lithos, 2014, 205:168-184.
[1] 孙文博, 苟军, 王世成, 王常东, 王广婷, 孙家兴, 张铎, 田丽, 孙德有. 大兴安岭南部白音沙那盆地中生代火山岩年代学及岩石成因[J]. 吉林大学学报(地球科学版), 2026, 56(3): 852-874.
[2] 张海洪, 乔锦燃, 陈国强, 薛晓刚, 邓馨卉, 苗长盛, 李 雪, 郜春生. 张广才岭南部早侏罗世两类I型花岗岩成因:年代学、地球化学和锆石Hf同位素证据[J]. 吉林大学学报(地球科学版), 2026, 56(3): 896-914.
[3] 徐骏, 高阳, 刘军, 王晓彤, . 大兴安岭北段三矿沟铁铜矿床成因——来自石榴子石U-Pb定年及元素地球化学证据[J]. 吉林大学学报(地球科学版), 2026, 56(2): 540-556.
[4] 高心如, 梁琛岳, 郑常青, 刘永江, 周建波, 宋志伟, 贾祥鹤, 殷浚哲, 洪雨萱, 谭卓, 张佳琦. 蒙古—鄂霍茨克构造域东段晚中生代演化历史——来自岩浆岩和沉积岩的证据[J]. 吉林大学学报(地球科学版), 2026, 56(1): 36-65.
[5] 孙宁辰, 周建波, 李功宇, 辛中华, 陈卓, 王红燕. 东北中生代盆地演化及其对古太平洋板块俯冲的制约[J]. 吉林大学学报(地球科学版), 2026, 56(1): 66-88.
[6] 蒋政, 舒彪, 路伟. 高温花岗岩张拉与剪切裂隙的渗流与传热性能试验[J]. 吉林大学学报(地球科学版), 2026, 56(1): 315-326.
[7] 戴振学, 李克英, 陈玮, 刘东. 北山花岗岩矿物的多尺度结构特征与智能识别[J]. 吉林大学学报(地球科学版), 2026, 56(1): 285-294.
[8] 唐华风, 付琦, 尹永康, 高有峰, 户景松, 武海超, 田志文. 花岗岩潜山储层地质研究回顾[J]. 吉林大学学报(地球科学版), 2025, 55(6): 1806-1836.
[9] 任云生, 徐文坦, 李京谋, 孙珍军, 刘干. 新疆东准地区黄羊山A型花岗岩形成时代与多阶段岩浆作用:来自SIMS锆石U-Pb年代学证据[J]. 吉林大学学报(地球科学版), 2025, 55(6): 1867-1884.
[10] 张国宾, 冯玥, 赵忠海, 宋学权, 何云龙, 孔金贵. 大兴安岭中段金江沟岩体侏罗纪花岗岩年代学、地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1564-1585.
[11] 陈琛昌, 唐宗源, 冯钊. 大兴安岭索伦地区早白垩世粗安岩与安山岩成因——来自地球化学和Sr-Nd-Hf同位素的约束[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1586-1607.
[12] 汪俊, 王哲, 李书华, 高红芳, 黄永健. 南海管事平顶海山密度结构及其构造意义[J]. 吉林大学学报(地球科学版), 2025, 55(5): 1691-1701.
[13] 尹业长, 姜朋, 郑博, 杨云宝, 李成禄, 刘阳, 刘兆龙, 刘旭显, 范玉超, 赵忠海.

大兴安岭北段库中地区早白垩世花岗岩锆石U-Pb年代学、地球化学特征及其地质意义 [J]. 吉林大学学报(地球科学版), 2025, 55(4): 1163-1180.

[14] 孙铭徽, 李向雨, 刘锦, 张洪祥, 董亚超, 张媛竹卉, 刘芸秀. 华北克拉通辽东半岛晚三叠世林家沟岩体的成因及构造意义[J]. 吉林大学学报(地球科学版), 2025, 55(3): 826-842.
[15] 曹锦山, 张新远, 欧阳光文, 王春涛, 刘建栋, 李五福.

松潘甘孜造山带南缘青海省秋智地区晚三叠世花岗岩体成因及构造背景  [J]. 吉林大学学报(地球科学版), 2025, 55(2): 483-502.

Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 于 平,李瑞磊,付 雷,郝 雪,张向军,廉国芬. 松辽盆地滨北地区区域构造特征及意义--地震长剖面给出的证据[J]. J4, 2005, 35(05): 611 -615 .
[2] 张原庆, 宋炳忠, 王玉福, 张宁. 鲁西铜石岩体金成矿规律和成矿预测[J]. J4, 2010, 40(6): 1287 -1294 .
[3] 李建平,李桐林,张 辉,徐凯军. 不规则回线源层状介质瞬变电磁场正反演研究及应用[J]. J4, 2005, 35(06): 790 -0795 .
[4] 高松, 宋莹, 王琳,蒋步新. 水体中秋兰姆特效降解菌的筛选及其降解性能研究[J]. J4, 2006, 36(03): 455 -457 .
[5] 张凤君,李 卿,马玖彤,于广菊. 膜蒸馏处理糠醛废水的实验研究[J]. J4, 2006, 36(02): 270 -0273 .
[6] 卢双舫,李吉君,薛海涛,徐立恒. 油成甲烷碳同位素分馏的化学动力学及其初步应用[J]. J4, 2006, 36(05): 825 -829 .
[7] 丁志宏,冯平,毛慧慧. 考虑径流年内分布影响的丰枯划分方法及其应用[J]. J4, 2009, 39(2): 276 -0280 .
[8] 任何军, 刘娜,高松,张兰英,张玉玲,周睿. 假单胞菌DN2对多氯联苯的降解及bphA1核心序列测定[J]. J4, 2009, 39(2): 312 -0316 .
[9] 黄奇波, 覃小群, 刘朋雨, 康志强, 唐萍萍. 半干旱区岩溶碳汇原位监测方法适宜性研究[J]. 吉林大学学报(地球科学版), 2015, 45(1): 240 -246 .
[10] 熊晓亮,孙红月,张世华,蔡岳良. 高扬程虹吸保障条件分析与合理管径选择数值模拟[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1595 -1601 .