吉林省下三叠统卢家屯组LA-ICP-MS锆石U-Pb定年及其地质意义

doi:10.13278/j.cnki.jjuese.201502110

摘要/Abstract

摘要：

卢家屯组按岩性组合自下而上分为影背山砾岩段、漏斗山杂色岩段、杨树河子黑色岩段,前人采集到的Palaeanodonta-Palaeomutela动物群、Pleuroneia? sp.和叶肢介等生物化石组合指示时代为二叠纪。本次对九台市影背山双顶山卢家屯组建组剖面下、中、上段进行了系统的碎屑锆石U-Pb同位素年代学研究,证实卢家屯组由下至上存在3个最小锆石年龄峰值,分别为(283.4±7.9)、(262.4±3.9)、(255.5±5.8) Ma,确定了卢家屯组的上限为晚二叠世。根据卢家屯组中碎屑锆石存在1 800 Ma和2 500 Ma左右的典型华北板块基底年龄,认为华北板块北缘与其北侧地块群最终闭合时间应为P₃-T₁。

关键词: 卢家屯组, 下三叠统, 碎屑锆石, LA-ICP-MS锆石U-Pb定年, 吉林省

Abstract:

According to the associated lithologic feature, the Lujiatun Formation is divided into Yingbeishan conglomerate section, Loudoushan variegated rock section, and Yangshuhezi black rock section. Based on the fossil assemblages, such as Palaeanodonta-Palaeomutela fauna, Pleuroneia? sp. and the conchostracan, it was formed in Permian. A systematic U-Pb isotopic chronology of the detrital zircon is studied for the Bottom, Middle, and Upper Section of the construction profiles of Lujiatun Formation in Yingbeishan-Shuangdingshan in Jiutai. The results show three minimum zircon age peaks at (283.4±7.9) Ma, (262.4±3.9) Ma, and (255.5±5.8) Ma from the bottom to the top. It can be confirmed that the top section of the formation belonged to the Late Permian. The detrital zircon ages of 1 800 Ma and 2 500 Ma in the Lujiantun Group are typical for the base plate age of North China Plate. In conclusion, the plate closure happened probably during P₃-T₁ between the northern margin of North China Plate and the group of plates to its north.

Key words: Lujiatun Formation, Lower Triassic, detrital zircon, zircon LA-ICP-MS U-Pb age, Jilin Province

中图分类号:

聂立军, 于宏斌, 张建泽, 王聪, 李栋, 李阳. 吉林省下三叠统卢家屯组LA-ICP-MS锆石U-Pb定年及其地质意义[J]. 吉林大学学报(地球科学版), 2015, 45(2): 453-470.

Nie Lijun, Yu Hongbin, Zhang Jianze, Wang Cong, Li Dong, Li Yang. Zircons LA-ICP-MS U-Pb Ages of the Lower Triassic Lujiatun Group and Its Geological Significance in Jilin Province[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(2): 453-470.

参考文献

[1] 李东津.吉林省岩石地层[M].北京:中国地质大学出版社, 1997:21-31. Li Dongjin. Jilin Rock Formations[M].Beijing: China University of Geosciences Press, 1997:21-31.

[2] 彭玉鲸, 齐成栋, 周晓东, 等.吉黑复合造山带古亚洲洋向滨太平洋构造域转换:时间标志与全球构造的联系[J].地质与资源, 2012, 21(3):261-265. Peng Yujing, Qi Chengdong, Zhou Xiaodong, et al. Ransition from Paleo-Asian Ocean Domain to Circum-Pacific Ocean Domain for the Ji-Hei Composite Orogenic Belt: Time Mark and Relationship to Global Tectonics[J].Geology and Resources, 2012, 21(3): 261-265.

[3] 王五力, 郭胜哲.中国东北古亚洲与古太平洋构造域演化与转换[J].地质与资源, 2012, 21(1):27-34. Wang Wuli, Guo Shengzhe. The Evolution and Transformation of Paleo-Asia and Paleo-Pacifictectonic Domain of Northeast China[J].Geology and Resources, 2012, 21(1): 27-34.

[4] 邵济安, 牟保磊, 何国琦, 等.华北北部在古亚洲域与古太平洋域构造叠加过程中的地质作用[J].中国科学:D辑, 1997, 27(5):390-394. Shao Ji'an, Mu Baolei, He Guoqi, et al. Geological Processes of the Process of Structural Overlapping Between Paleo-Asian Domain and Paleo-Pacific Domain in Northern Part of North China[J].Science in China:Series D, 1997, 27(5):390-394.

[5] 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.

[6] Miao L C, Fan W M, Liu D Y, et al. Geochronology and Geochemistry of the Hegenshan Ophiolitic Complex: Implications for Late-Stage Tectonic Evolution of the Inner Mongolia-Daxinganling Orogemc Belt, China[J]. Journal of Asian Earth Sciences, 2008, 32:348-370.

[7] 王玉净, 樊志勇.内蒙古西拉木伦河北部蛇绿岩带中二叠纪放射虫的发现及其地质意义[J].古生物学报, 1997, 36(1):58-69. Wang Yujing, Fan Zhiyong. Discovery of Permian Radiolarians in Ophiolite Belt on Northern Side of Xar Moron River, Nei Monggol and Its Geological Significance[J].Acta Palaeontologica Sinica, 1997, 36(1): 58-69.

[8] 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. Significant Achievements and Open Issues in Study of Orogenesis and Metallogenesis Surrounding the North China Continent[J].Acta Petrologica Sinica, 2009, 25(11):2695-2726.

[9] 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 Sys-Clooisional 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 Sinica, 2007, 23(3):565-582.

[10] 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.

[11] 郗爱华, 任洪茂, 张宝福, 等.吉林中部呼兰群同位素年代学及其地质意义[J].吉林大学学报:地球科学版, 2003, 33(1):15-18. Xi Aihua, Ren Hongmao, Zhang Baofu, et al.Isotopic Chronology of the Hulan Group and Its Geological Significance in the Central Jilin Province[J].Journal of Jilin University: Earth Science Edition, 2003, 33(1):15-18.

[12] Andersen T. Correction of Common Lead in U-Pb Analyses that Do not Report ²⁰⁴Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.

[13] Ludwing K R. Using Isoplot/Ex, Version 2.49: A Geochronological Toolkit for Microsoft Excel[M].Berkeley: Berkeley Geochronological Center Special Publiction, 2001:1-55.

[14] Yuan H L, Gao S, Liu X M, et al. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation Inductivey Coupled Plasma Mass Spectrometry[J].Geastandard Newsletter, 2004, 28(3):353-370.

[15] Koschek G. Origin and Significance of the SEM Cathodoluminescence from Zircon[J].Journal of Microscopy, 1993, 171(3):223-232.

[16] Leiss O. Orogenically Controlled Sedimentation in the Lechtaler Kreideschiefer(Lechtal Shale: Cretaceous) and Geodynamics of Inner Western CA(Northern Calearous Alps: Leehatl Alps)[J]. Geological Rundschau, 1992, 81(3):603-634.

[17] 肖庆辉, 李晓波, 贾跃明, 等.当代造山带研究中值得重视的若干前沿问题[J].地学前缘, 1995, 2(1/2):43-50. Xiao Qinghui, Li Xiaobo, Jia Yueming, et al. Frontiers on Orogenic Belt Researches[J].Earth Science Frontiers, 1995, 2(1/2):43-50.

[18] 闫义, 林舸, 李自安.利用锆石形态、成分组成及年龄分析进行沉积物源区示踪的综合研究[J].大地构造与成矿学, 2003, 27(2):184-190. Yan Yi, Lin Ge, Li Zian. Provenance Tracing of Sediments by Means of Synthetic Study of Shape, Composition and Chronology of Zircon[J].Geotectonica et Metallogenia, 2003, 27(2):184-190.

[19] 韩国卿, 刘永江, 温泉波, 等.西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义[J].地球科学:中国地质大学学报, 2011, 36(4):687-702. Han Guoqing, Liu Yongjiang, Wen Quanbo, et al. LA-ICP-MS U-Pb Dating of Detrital Zircons from the Permian Sandstones in North Side of Xar Moron River Suture Belt and Its Tectonic Implications[J].Earth Science:Journal of China University of Geosciences, 2011, 36(4):687-702.

[20] 梁爽, 彭玉鲸, 姜正龙.松辽盆地基底"多层结构"的探讨及其构造意义[J].世界地质, 2009, 28(4):430-437. Liang Shuang, Peng Yujing, Jiang Zhenglong. Discussion on "Multi-Laminate Structure" of Basement in Songliao Basin and Its Significance[J].Global Geology, 2009, 28(4):430-437.

[21] 许文良, 王枫, 孟恩, 等.黑龙江省东部古生代早中生代的构造演化:火成岩组合与碎屑锆石U-Pb年代学证据[J].吉林大学学报:地球科学版, 2012, 42(5):1378-1389. Xu Wenliang, Wang Feng, Meng En, et al. Paleozoic-Early Mesozoic Tectonic Evolution in the Eastern Heilongjiang Province, NE China:Evidence from Igneous Rock Association and U-Pb Geochronology of Detrital Zircons[J].Journal of Jilin University: Earth Science Edition, 2012, 42(5):1378-1389.

[22] 李俊建, 沈保丰, 李双保, 等.辽北吉南早前寒武纪大陆壳的地质特征和演化[J].中国区域地质, 1998, 17(1):30-38. Li Junjian, Shen Baofeng, Li Shuangbao, et al. 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.

[23] 吴福元, 葛文春, 孙德有, 等.吉林南部太古代花岗岩Sm-Nd, Rb-Sr同位素年龄测定[J].岩石学报, 1997, 13(4):499-506. Wu Fuyuan, Ge Wenchun, Sun Deyou, et al. The Sm-Nd, Rb-Sr Isotopic Ages of the Archean Granites in Southern Jilin Province[J].Acta Petrologica Sinica, 1997, 13(4):499-506.

[24] 毕守业, 张殿发, 杨豹.吉林省南部太古宙花岗质岩石及其成因探讨[J].吉林地质, 1991(3):12-24. Bi Shouye, Zhang Dianfa, Yang Bao. A Prelininary Study Archaean Granitic Rocks and Its Origin in the Southern Part of Jilin Province[J].Jilin Geology, 1991(3):12-24.

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