吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 389-403.doi: 10.13278/j.cnki.jjuese.201502105

• 地质与资源 • 上一篇    下一篇

大兴安岭中段柴河地区玛尼吐组火山岩年代学、地球化学及岩石成因

司秋亮1,2, 崔天日2, 唐振2,3, 李伟2, 吴新伟2,3, 江斌2,3, 李林川2,3   

  1. 1. 东北大学资源与土木工程学院, 沈阳 110819;
    2. 沈阳地质矿产研究所/中国地质调查局沈阳地质调查中心, 沈阳 110034;
    3. 吉林大学地球科学学院, 长春 130061
  • 收稿日期:2014-07-16 发布日期:2015-03-26
  • 作者简介:司秋亮(1982-),男,博士研究生,工程师,主要从事火山岩方面的研究,E-mail:siqiuliang@126.com
  • 基金资助:

    高等学校博士学科点专项科研基金项目(20110042110032);中国地质调查局区域地质大调查项目(12120113053800,1212011085210)

Chronology,Geochemistry and Petrogenesis of the Volcanic Rocks in Manitu Formation in Chaihe Area, Central Great Xing'an Range

Si Qiuliang1,2, Cui Tianri2, Tang Zhen2,3, Li Wei2, Wu Xinwei2,3, Jiang Bin2,3, Li Linchuan2,3   

  1. 1. College of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China;
    2. Shenyang Institute of Geology and Mineral Resources/Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
    3. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2014-07-16 Published:2015-03-26

PDF (PC)

497

摘要：

对大兴安岭中段柴河地区玛尼吐组火山岩进行了锆石LA-ICP-MS U-Pb年代学和岩石地球化学研究,以了解其形成时代、岩石成因及其所揭示的区域构造背景。玛尼吐组火山岩岩相学鉴定结果为安山岩、英安岩,化学成分显示其为粗面英安岩、粗面岩和英安岩。玛尼吐组火山岩锆石多呈自形半自形晶,振荡环带发育,Th/U=0.33~2.08,指示其岩浆成因。定年结果显示,玛尼吐组火山岩形成于139~148 Ma的晚侏罗世。岩石地球化学研究表明,玛尼吐组火山岩的w(SiO2)为64.87%~68.65%,w(Al2O3)为15.53%~16.72%,全碱w(Na2O+K2O)为6.75%~9.22%,K2O/Na2O=0.63~1.57,属于高钾钙碱性系列。所有样品的稀土配分曲线具有相似的特征,稀土丰度总量w(∑REE)为(124.95~208.57)×10-6,轻重稀土分馏明显,(La/Yb)N=11.50~14.88, Eu负异常(0.45~1.17),微量元素以富集Rb、Ba、K,亏损Nb、P、Ti为特征。玛尼吐组火山岩原始岩浆来源于地壳岩石的部分熔融,形成于蒙古-鄂霍茨克缝合带闭合后的岩石圈伸展构造环境。

关键词: LA-ICP-MS锆石U-Pb定年, 地球化学, 火山岩, 玛尼吐组, 柴河地区, 大兴安岭中段

Abstract:

The zircon LA-ICP-MS U-Pb dating and geochemistry are reported for the volcanic rocks in Manitu Formation in Chaihe, central Great Xing'an Range in order to discover its formation time, petrogenesis and the regional tectonic setting Petrographically.The volcanic rocks in Manitu Formation are composed of andesite and dacite,but they are trachyte, trachydacite, and dacite based on its chemical composition. Zircon from these volcanic rocks are euhedral-subhedral in shape, with fine-scale oscillatory growing ring. The Th/U ratio of (0.33-2.08) indicates a magmatic origin. The dating results show that the volcanic rocks in Manitu Formation are formed in Late Jurassic from 139 to 148 Ma. The geochemical study shows that the SiO2 of the andesite is between 64.87%-68.65%,Al2O3 is between 15.53%-16.72%,Na2O+K2O is between 6.75%-9.22%,K2O/Na2O is between 0.63-1.57, falling in the series of high-potassium calc-alkaline. All samples have a similar REE pattern with a significant fractionation of LREE from HREE((La/Yb)N =11.50-14.88)and negative Eu anomalies(δEu=0.45-1.17). The total rare earth element is from 124.95×10-6 to 208.57×10-6. The trace element geochemistry is characterized evidently by enrichment of Rb, Ba, K, depletion of Nb, P, Ti. Its original magma is derived from the partial melting of the crust,during an extension after the closure of the Mongol-Okhotsk Ocean.

Key words: LA-ICP-MS zircon U-Pb dating, geochemistry, volcanic rocks, Manitu Formation, Chaihe area, Central Great Xing'an Range

中图分类号: 

  • P588.141

[1] 葛文春, 李献华, 林强, 等. 呼伦湖早白垩世碱性流纹岩的地球化学特征及其意义[J].地质科学, 2001, 36(2):176-183. Ge Wenchun, Li Xianhua, Lin Qiang, et al. Geochemistry of Early Cretaceous Alkaline Andesite from Hulun Lake, Daxing'anling and Its Tectonic Implications[J]. Scientia Geologica Sinica, 2001, 36(2):176-183.

[2] 赵忠华, 孙德友, 苟军, 等.满洲里南部塔木兰沟组火山岩年代学与地球化学[J]. 吉林大学学报:地球科学版, 2011, 41(6):1866-1880. Zhao Zhonghua, Sun Deyou, Gou Jun, et al. Chronology and Geochemistry of Volcanic Rocks in Tamulangou Formantion from Southern Manchuria, Inner Mongolia[J].Journal of Jilin University:Earth Science Edition, 2011, 41(6): 1866-1880.

[3] 林强, 葛文春, 曹林, 等. 大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学, 2003, 32(3): 208-222. Lin Qiang, Ge Wenchun, Cao Lin, et al. Geochemistry of Mesozoic Volcanic Rocks in Da Hinggan Ling: The Bimodal Volcanic Rocks[J]. Geochimica, 2003, 32(3):208-222.

[4] Wang Feng, Zhou Xinhua, Zhang Lianchang, 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, 251:179-198.

[5] 张振强.额尔古纳满洲里地区中生代火山岩与铀成矿地质条件研究[J].辽宁地质, 2000, 17(4):263-266. Zhang Zhenqiang.Study on Mesozoic Volcanic Rocks and Uranium Metallogenic Geological Conditions in Erguna-Manzhouli[J]. Liaoning Geology, 2000, 17(4):263-266.

[6] Zhang Jiheng, Ge Wenchun, Wu Fuyuan, et al. Large Scale Early Cretaceous Volcanic Events in the Northern Great Xing'an Range, Northeastern China[J].Lithos, 2008, 102(1/2):138-157.

[7] Zhang Jiheng, Gao Shan, Ge Wenchun, et al. Geochronology of the Mesozoic Volcanic Rocks in the Great Xing'an Range, Northeastern China: Implications for Subduction-Induced De Lamination[J]. Chemical Geology, 2010, 276(3/4):144-165.

[8] Meng En, Xu Wenliang, Pei Fuping. Chronology of Late Paleozoic Volcanism in Eastern and Southeastern Margin of Jiamusi Massif and Its Tectonic Implications[J].Chinese Sciences Bulletin, 2008, 53:1231-1245.

[9] 苟军, 孙德有, 赵忠华, 等.满洲里南部玛尼吐组安山岩锆石U-Pb定年及岩石成因[J].岩石学报, 2010, 26(1):333-344. Gou Jun, Sun Deyou, Zhao Zhonghua, et al. Zircon LA-ICP-MS U-Pb Dating and Petrogenesis of Andesite in Manitu Formation from the Southern Manzhouli, Inner Mongolia[J]. Acta Petrologica Sinica, 2010, 26(1):333-344.

[10] Ying Jifeng, Zhou Xinhua, Zhang Lianchang, et al.Geochronological Framwork of Mesozoic Volcanic Rocks in the Great Xing'an Range, NE China, and Their Geodynamic Implications[J]. Journal of Asian Earth Sciences, 2010, 39(6):786-793.

[11] 孟恩, 许文良, 杨德彬, 等.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其他地质意义[J].岩石学报, 2011, 27(4):1209-1226. Meng En, Xu Wenliang, Yang Debin, et al. Zircon U-Pb Chronology, Geochemistry of Mesozoic Volcanic Rocks from Lingquan Basin in Manzhouli Area, and Its Tectonic Implications[J]. Acta Petrologica Sinca, 2011, 27(4):1209-1226.

[12] 徐美君, 许文良, 孟恩, 等.内蒙古东北部额尔古纳地区上护林向阳盆地中生代火山岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J].地质通报, 2011, 30(9):1321-1338. Xu Meijun, Xu Wenliang, Meng En, et al. LA-ICP-MS Zircon U-Pb Chronology and Geochemistry of Mesozoic Volcanic Rocks from the Shanghulin-Xiangyang Basin in Erguna Area, Northeastern Inner Mongolia[J]. Geological Bulletin of China, 2011, 30(9):1321-1338.

[13] 孙德有, 苟军, 任云生, 等. 满洲里南部玛尼吐组火山岩锆石U-Pb年龄与地球化学研究[J].岩石学报, 2011, 27(10):3083-3094. Sun Deyou, Gou Jun, Ren Yunsheng, et al.Zircon U-Pb Dating and Study on Geochemistry of Volcanic Rocks in Manitu Formation from Southern Manchuria, Inner Mongolia[J]. Acta Petrologica Sinica, 27(10):3083-3094.

[14] 孙巍, 迟效国, 潘世语, 等. 大兴安岭北部新林地区倭勒根群大网子组锆石LA-ICP-MS U-Pb年龄及其地质意义[J].吉林大学学报:地球科学版, 2014, 44(1):176-185. Sun Wei, Chi Xiaoguo, Pan Shiyu, et al. Zircon LA-ICP-MS U-Pb Dating and Significance of Da-wangzi Formation from Wolegen Group in Xinlin Area, Northern Great Xing'an Range[J]. Journal of Jilin University:Earth Science Edition, 2014, 44(1):176-185.

[15] 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.

[16] 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 Erolution of the Mesozoil Volcanism in Mid-Southern Daxing'anling Mountain[J]. Regional Geology of China, 1999, 18(4): 351-358.

[17] 杨扬, 高福红, 陈井胜, 等.赤峰地区中生代火山岩锆石U-Pb年代学证据[J].吉林大学学报:地球科学版, 2012, 42(增刊2):257-268. Yang Yang, Gao Fuhong, Chen Jingsheng, et al. Zircon U-Pb Ages of Mesozoic Volcanic Rocks in Chifeng Area[J]. Journal of Jilin University:Earth Science Edition, 2012, 42(Sup.2):257-268.

[18] Zhang Jiheng, Ge Wenchun, Wu Fuyuan, et al. Mesozoic Bimodal Volcanic in Zhalantun of the Da Hinggan Range and Its Geological Significance: Zircon U-Pb Age and Hf Isotopic Constraints.Acta[J].Geologica Sinica, 2006, 80(1):58-69.

[19] 崔天日, 杨芳林, 司秋亮, 等.大兴安岭中段柴河地区碎斑熔岩的发现及其意义[J].地质与资源, 2012, 21(1):35-41. Cui Tianri, Yang Fanglin, Si Qiuliang, et al. Discovery and Significance of the Porphyroclastic Lava in Chaihe Area, Middle Daxinganling Moutains[J]. Geology and Resources, 2012, 21(1):35-41.

[20] 王建国, 和钟铧, 许文良. 大兴安岭南部钠闪石流纹岩的岩石成因:年代学和地球化学证据[J].岩石学报, 2013, 29(3):853-863. Wang Jianguo, He Zhonghua, Xu Wenliang. Petrogenesis of Riebecki Rhyolotes in the Southern Da Hinggan Mts: Geochronological and Geochemical Evidence[J]. Acta Petrologica Sinca, 2013, 29(3):853-863.

[21] 李世超, 徐仲元, 刘正宏, 等. 大兴安岭中段玛尼吐组火山岩LA-ICP-MS锆石U-Pb年龄及地球化学特征[J].地质通报, 2013, 32(2):199-207. Li Shichao, Xu Zhongyuan, Liu Zhenghong, et al. Zircon U-Pb Dating and Geochemical Study of Volcanic Rocks in Manitu Formation of Central Da Hinggan Mountains[J]. Geological Bulletin of China, 2013, 32(2): 199-207.

[22] Jackson S E, Pearson N J, Griffin W L, et al. The Application of Laser Ablation-Inductively Coupled Plasma-Mass Spec-Trometry(LA-ICP-MS)to in Situ U-Pb Zircon Geochronology[J]. Chem Geol, 2004, 211:47-69.

[23] Andersen T. Correction of Common Lead in U-Pb Analyses that do not Report 204Pb[J]. Chemical Geology, 2002, 192:59-79.

[24] Ludwig K R. ISOPLOT 3:A Gochronological Toolkit for Microsoft Excel[M]. Berkeley:Special Publication, 2003.

[25] Yuan Honglin, Gao Shan, Liu Xiaoming et al. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Blation Inductively Coupled Plasma Mass Spectrometry[J]. Geostandard Newsletter:The Journal of Geostandards and Geoanalysis, 2004, 28:353-370.

[26] Middlemost E A K. Magmas and Magmatic Rocks: An Introduction to Igneous Petrology[M]. London: Longman Group, 1985.

[27] Irvine T N, Baragar W R. A Guide to the Chemical Classification of the Common Volcanic Rocks[J]. Canadian Journal of Earth Sciences, 1971, 8:523-548.

[28] Peccerillo A, Taylor T S. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from Kastamonu Area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58:63-81.

[29] Sun S S, McDonough W F. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Process[C]//Sauders A D, Norry M J.Magmatism in the Ocean Basins.Geolo-gical Society Special Publication, 1989, 42:313-345.

[30] Rittman A. Note to Contribution by V Gottini on the "Serial Character of the Volcanic Rocks of Pantelleria"[J]. Bull Volcanol, 1970, 33:978-981.

[31] 许文良, 葛文春, 裴福萍, 等.东北地区中生代火山作用的年代学格架及其构造意义[J].矿物岩石地球化学通报, 2008, 27(增刊1):286-287. Xu Wenliang, Ge Wenchun, Pei Fuping, et al. Geochronological Framwork of Mesozoic Volcanic Rocks in NE China and Its Tectonic Implications[J].Bulletin of Minerallgy, Petrology and Geochemistry, 2008, 27(Sup.1):286-287.

[32] 张吉衡.大兴安岭中生代火山岩年代学及地球化学研究.北京:中国地质大学, 2009. Zhang Jiheng. Geochronology and Geochemistry of the Mesozoic Volcanic Rocks in the Great Xing'an Range, Northeastern China. Beijing:China University of Geosciences, 2009.

[33] 陈志广, 张连昌, 吴华英, 等.二连盆地北缘晚中生代火山岩Ar-Ar年代、地球化学及构造背景[J].岩石学报, 2009, 25(2):297-310. Chen Zhiguang, Zhang Lianchang, Wu Huaying, et al. Ar-Ar Age, Geochemistry and Petrogenesis of Late Mesozoic Volcanic Rocks in the Northern Marginal Region of Erlian Basin, Inner Mongolia[J]. Acta Petrologica Sinica, 2009, 25(2):297-310.

[34] Pearce J A.The Role of Sub-continental Lithosphere in Magma Genesisi at Destructive Plate Margins[C]//Hawkesworth C J, Norry M J.Continental Basalts and Mantle Xenoliths.Nantwich Shiva:Academic Press, 1983:230-249.

[35] 徐公愉.大兴安岭的大陆火山岩及其矿化作用[J].地质通报, 1983(3): 39-50. Xu Gongyu.Continental Volcanic Rocks in the Greater Khingan Mountains and Their Mineralization[J].Geological Bulletin of China, 1983(3): 39-50.

[36] 蒋国源, 权恒.大兴安岭根河海拉尔盆地中生代火山岩[J].中国地质科学院沈阳地质矿产研究所所刊, 1988(3): 23-100. Jiang Guoyuan, Quan Heng. Mesozoic Volcanic Rock of Genhe and Hailaer Basins in Daxinganling[J]. Bulletin of Shenyang Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 1988(3):23-100.

[37] 夏军, 王成善, 李秀华, 等.海拉尔及其邻区中生代火山岩的特征与边缘陆块型火山岩的提出[J]. 成都地质学院学报, 1993, 20(4):67-80. Xia Jun, Wang Chengshan, Li Xiuhua, et al.Characteristics of Mesozoic Volcanic Rocks in Hailaer and Its Adjacent Areas and Discussion on Volcanic Rocks of Marginal Block Type[J]. Journal of Chengdu College of Geology, 1993, 20(4):67-80.

[38] 许文良, 孙德有, 周燕.满洲里绥芬河地学断面岩浆作用和地壳结构[M]. 北京: 地质出版社, 1994. Xu Wenliang, Sun Deyou, Zhou Yan. Manzhouli-Suifenhe Geoscience Transect: Magmatism and Crust Structure[M].Beijing: Geological Publishing House, 1994.

[39] 邓晋福, 赵海玲, 莫宣学, 等.中国大陆根柱构造:大陆动力学的钥匙[M].北京:地质出版社, 1996. Deng Jinfu, Zhao Hailing, Mo Xuanxue, et al.Continental Roots-Plume Tectonics of China: Key to the Continental Dynamics[M]. Beijing: Geological Publishing House, 1996.

[40] 董树文, 吴锡浩, 吴珍汉, 等.论东亚大陆的构造翘变: 燕山运动的全球意义[J].地质论评, 2000, 46(1):8-13. Dong Shuwen, Wu Xihao, Wu Zhenhan, et al. On Tectonic Seesawing of the East Asia Continent: Global Implication of the Yanshanian Movenment[J]. Geological Review, 2000, 46(1):8-13.

[41] 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 Daxing'anling[J].Earth Science Frontiers, 1999, 6(4):339-346.

[42] 马家骏, 方大赫.黑龙江省中生代火山岩初步研究[J].黑龙江地质, 1991, 2(2):1-16. Ma Jiajun, Fang Dahe.A Preliminary Study of the Mesozoic Volcanic Rocks in Heilongjiang Province, China[J].Heilongjiang Geology, 1991, 2(2): 1-16.

[43] 朱勤文, 路凤香, 谢意红, 等. 大陆边缘扩张型活动带火山岩组合:松辽盆地周边中生代火山岩研究[J].岩石学报, 1997, 13(4):551-562. Zhu Qinwen, Lu Fengxiang, Xie Yihong, et al. Volcanic Assemblages in Active Belt of Spreading Type in Continental Margin: Study on Mesozoic Volcanic Rocks Around Songliao Basin[J]. Acta Petrologica Sinica, 1997, 13(4):551-562.

[44] Griffin W L, Zhang A D, O'Reilly S Y, et al.Phanerozoic Evolution of the Lithosphere Beneath the Sino-Korean Craton[C]//Flower M F J, Chung S L, Lo C H, et al. Mantle Dynamics and Plate Interactions in East Asia.Am Geophys Union Geogyn Ser, 1998, 27:107-126.

[45] Menzie M A, Xu Y. Geodynamics of the North China Craton[C]//Flower M F J, Chung S L, Lo C H, et al.Mantle Dynamics and Plate Interactions in East Asia.Geodynamics Series, 1998, 27:155-165.

[46] 吴福元, 孙德有, 张广良, 等.论燕山运动的深部地球动力学本质[J]. 高校地质学报, 2000, 6(3):379-388. Wu Fuyuan, Sun Deyou, Zhang Guangliang, et al. Deep Geodynamics of Yanshan Movement[J].Geological Journal of China Univerisities, 2000, 6(3):379-388.

[47] 林强, 葛文春, 孙德有, 等中国东北地区中生代火山岩的大地构造意义[J].地质科学, 1998, 33(2):129-139. Lin Qiang, Ge Wenchun, Sun Deyou, et al. Tectonic Significance of Mesozoic Volcanic Rocks in Nor-theastern China[J]. Scientia Geologica Sinica, 1998, 33 (2):129-139.

[48] 葛文春, 林强, 孙德有, 等.大兴安岭中生代两类流纹岩成因的地球化学研究[J]. 地球科学, 2000, 25(2):172-178. Ge Wenchun, Lin Qiang, Sun Deyou, et al. Geo-Chemical Research into Origins of Two Types of Mesozoic Andesite in Daxing'anling[J]. Earth Science, 2000, 25(2):172-178.

[49] Wang Pujun, Liu Wanzhu, Wang Shuxue et al.40Ar-39Ar and K-Ar Dating on the Volcanic Rocks in the Songliao Basin, NE China:Constraints on Stratigraphy and Basin Dynamics Int[J]. Earth Sci, 2002, 91:331-340.

[50] 周新华, 英基丰, 张连昌, 等.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U-Pb年龄及多元同位素制约[J]. 地球科学:中国地质大学学报, 2009, 34(1):1-10. Zhou Xinhua, Ying Jifeng, Zhang Lianchang, et al. The Petrogenesis of Late Mesozoic Volcanic Rock and the Contributions from Ancient Micro-Continents: Constraints from the Zircon U-Pb Dating and Sr-Nd-Pb-Hf Isotopic Systematics[J].Earth Science:Journal of China University of Geosciences, 2009, 34(1):1-10.

[51] Xu Wenliang, Ji Weiqiang, Pei Fuping, et al. Triassic Volcanism in Eastern Heilongjiang and Jilin Provinces, NE China:Chronology, Geochemistry, and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2009, 34(3):392-402.

[52] Fan Weiming, Guo Feng, Wang Yuejun. Late Mesozoic Calc-Alkaline Volcanism of Post-Orogenic Extension in the Northern Da Hingan Mountains, Northeastern China[J]. Journal of Volcanology and Geothermal Research, 2003, 121:115-135.

[53] Zorin Y A. Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt, Trans-Baikal Region(Russia) and Mongolia[J].Tectonophysics, 1999, 306:33-56.

[54] Metelkin D V, Vernikovsky V A, Kazansky A Y, et al. Late Mesozoic Tectonics of Central Asia Based on Paleomagnetic Evidence[J].Gondwana Research, 2010, 18(2/3):400-419.

[55] Zhang Yueqiao, Dong Shuwen, Zhao Yue, et al. Jurassic Tectonics of North China:A Synthetic View[J]. Acta Geologica Sinica, 2008, 82(2):310-326.

[56] 邱家骧, 林景仟.岩石化学[M]. 北京: 地质出版社, 1993. Qiu Jiaxiang, Lin Jingqian. Petrochemistry[M].Beijing: Geological Publishing House, 1993.

[57] Muller D, Rock N M S, Groves D I. Geochemical Discrimination Between Shoshonitic and Potassic Volvanic Rocks in Different Tectonic Settings:A Pilot Study[J].Mineralogy and Petrology, 1992, 46:259-289.
[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] 舒晴, 朱晓颖, 高维, 李瑞, 尹航. 三塘湖盆地航磁异常特征及油气远景预测[J]. 吉林大学学报(地球科学版), 2018, 48(2): 451-460.
[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] 刘宗利, 王祝文, 刘菁华, 赵淑琴, 欧伟明. 辽河东部凹陷火山岩相测井响应特征及储集意义[J]. 吉林大学学报(地球科学版), 2018, 48(1): 285-297.
[11] 潘保芝, 刘文斌, 张丽华, 郭宇航, 阿茹罕. 一种提高储层裂缝识别准确度的方法[J]. 吉林大学学报(地球科学版), 2018, 48(1): 298-306.
[12] 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.
[13] 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.
[14] 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.
[15] 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.
Viewed
Full text
282
HTML PDF
Just accepted Online first Issue Just accepted Online first Issue
0 0 0 0 0 282

  From Others local
  Times 145 137
  Rate 51% 49%

Abstract
504
Just accepted Online first Issue
0 0 504
  From Others local
  Times 439 65
  Rate 87% 13%

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