吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 405-424.doi: 10.13278/j.cnki.jjuese.20190324

• 沉积盆地分析 • 上一篇    下一篇

大兴安岭索伦地区哲斯组碎屑岩地球化学特征和锆石U-Pb年龄对沉积物源属性约束

和钟铧, 王启智, 王强   

  1. 吉林大学地球科学学院, 长春 130061
  • 收稿日期:2019-12-30 出版日期:2020-03-26 发布日期:2020-03-31
  • 作者简介:和钟铧(1968-),男,教授,博士生导师,主要从事构造地质学方面的研究,E-mail:hezhonghua@126.com
  • 基金资助:
    中国地质调查局地质调查项目(12120114012901)

Geochemistry and Zircon U-Pb Ages of Clastic Rocks of Zhesi Formation in Suolun Region, Great Xing’an Range: Constraints on Origins of Sediment Provenance

He Zhonghua, Wang Qizhi, Wang Qiang   

  1. College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2019-12-30 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by Geological Survey Project of China Geological Survey(12120114012901)

摘要: 本文以内蒙古索伦地区好仁镇出露良好的中二叠世哲斯组碎屑岩为研究对象,利用碎屑岩地球化学特征和锆石年代学等示踪技术分析哲斯组沉积物源的年代和性质。测年结果显示,哲斯组砂岩碎屑锆石U-Pb年龄分为6组:282~244、352~294、468~379、513~482、802~580、2 500~1 800 Ma。碎屑岩地球化学具有高SiO2和低Fe2O3、FeO、MgO质量分数的特点,说明其母岩为长英质岩石。稀土、微量元素特征及其构造图解显示,哲斯组沉积物源区多具有大陆岛弧型和活动大陆边缘型的特点,少量反映被动大陆边缘的特点。对比研究显示,沉积物源区所反映的大陆岛弧型和活动大陆边缘型的构造环境是不同时期佳-蒙地块拼合碰撞和古亚洲洋南支北向俯冲的结果,少量所反映的被动大陆边缘环境可能是部分基底岩石形成时构造环境的响应。鉴于研究区位于兴安地块东南部,远离华北地块,且哲斯组碎屑岩多为长石岩屑砂岩、岩屑长石砂岩、岩屑砂岩,其结构成熟度和成分成熟度较低,显示近源沉积的特点,与其同期的火成岩均显示岛弧或活动大陆边缘的构造背景,据此推测哲斯组应形成于古亚洲洋南支向佳-蒙地块俯冲形成的弧后或弧间盆地环境,物源主要来自于佳-蒙地块南缘与岛弧或活动大陆边缘有关的火成岩,少量来自于佳-蒙地块的古老基底。

关键词: 碎屑锆石年龄, 地球化学, 物源分析, 哲斯组, 内蒙古索伦地区

Abstract: This paper focused on the clastic rocks of the Middle Permian Zhesi Formation, well exposed in the Haoren Town, Suolun region of Inner Mongolia. Geochemistry and zircon geochronology analyses were conducted, in order to constrain the ages and origins of sediment provenance. The dating results show that the U-Pb ages of detrital zircons from the Zhesi Formation sandstone can be divided into six groups, i.e., 282-244 Ma, 352-294 Ma, 468-379 Ma, 513-482 Ma, 802-580 Ma, and 2 500-1 800 Ma, respectively. Geochemically, the sandstone samples have high SiO2, and low Fe2O3, FeO, and MgO contents, indicating they were mainly deposited from felsic rocks. Rare earth elements and trace elements characteristics and tectonic distinguished diagrams suggest the sediment source region of the Middle Permian Zhesi Formation dominantly displays similar features with those of continental arc and active continental margin, with minor corresponding to passive continental margin. The former setting is the results of the amalgamation-collision of the Jiamusi-Mongolia block and northwards subduction of the south branch of the Paleo-Asian Ocean during different stages, while the later one probably reflects the tectonic setting of the generation of some basement rocks. Considering the facts that:1) the study region is located in the southeastern Xing'an block, far away form the North China craton; 2) the Zhesi Formation clastic rocks mainly consist of feldspar lithic sandstone, lithic feldspar sandstone, and lithic sandstone with relatively low structure and ingredient maturity, suggesting characteristics of near-source deposition; and 3) the coeval igneous rocks in the surrounding regions were all formed in subduction-related settings, it is proposed here that the Zhesi Formation was most likely deposited in a back-arc or inter-arc basin related with the northwards subduction of the south branch of the Paleo-Asian Ocean beneath the Jiamusi-Mongolia block, and their provenance was dominantly from the subduction-related igneous rocks in the southern margin of the Jiamusi-Mongolia block, with little contributions from ancient basement of the Jiamusi-Mongolia block.

Key words: detrital zircon ages, geochemistry, provenance analyses, Zhesi Formation, Suolun region of Inner Mongolia

中图分类号: 

  • P588.2
[1] 李勇,王成善,曾允孚. 造山作用与沉积响应[J].矿物岩石,2000, 20(2):19-56. Li Yong, Wang Chengshan, Zeng Yunfu. Orogeny and Sedimentary Response[J]. Journal Mineralogy and Petrology, 2000, 20(2):19-56.
[2] Bhatia M R.Plate Tectonics and Geochemical Composition of Sandstones[J]. The Journal of Geology, 1983, 91(6):611-627.
[3] Weltje G J, Von E H. Quantitative Provenance Analysis of Sediments:Review and Outlook[J]. Sedimentary Geology, 2004, 171(1/2/3/4):1-11.
[4] Mark W H, Rew C M. Evaluation of Sediment Provenance Using Magnetic Mineral Inclusions in Clastic Silicates:Comparison with Heavy Mineral Analysis[J]. Sedimentary Geology, 2004, 171:13-36.
[5] Dickinson W R, Suczek C A. Plate Tectonics and Sandstone Compositions[J]. American Association of Petroleum Bulletin, 1979, 63(2):2164-2182.
[6] Dickinson W R. Provenance of North American Phanerozoic Sandstones in Relation to Ttectonic Setting[J]. Bulletin Geological of Society America, 1983, 94:222-235.
[7] Schwab F L. Evolution of the Western Continental Margin, French-Italian Alps:Sandstone Mineralogy as an Iindex of Plate Tectonic Setting[J]. Journal of Geology, 1981, 89(3):349-368.
[8] Roser B P, Korsch R J. Determination of Tectonic Setting of Sandstone Mud Stone Suites Using SiO2 Content and K2O/Na2O Ratio[J]. Journal of Geology, 1986, 94(5):635-650.
[9] Darby B J, George G. Detrital Zircon Reference for the North China Block[J]. Journal of Asian Earth Sciences, 2006, 26:637-648.
[10] Monika A K, Artur K, Mariusz P, et al. Provenance Implications of Th-U-Pb Electron Microprobe Ages from Detrital Monazite in the Carboniferous Upper Silesia Coal Basin, Oland[J]. Lithos, 2006, 88:56-71.
[11] 杨文涛,杨江海,汪校锋,等. 豫西济源盆地中三叠世-中侏罗世碎屑锆石年代学及其对秦岭造山带造山过程的启示[J]. 地球科学:中国地质大学学报,2012, 37(3):489-500. Yang Wentao, Yang Jianghai, Wang Xiaofeng, et al. Geochronology from Middle Triassic to Middle Jurassic Detrital Zirons in Jiyuan Basin and Its Implications for the Qinling Orogen[J]. Earth Science:Journal of China University of Geosciences, 2012, 37(3):489-500.
[12] 徐严,颜林杰,张佳明,等. 中亚造山带东段晚古生代伸展构造环境的证据:内蒙古双井地区哲斯组沉积学及年代学研究[J]. 岩石学报,2018, 34(10):3052-3070. Xu Yan,Yan Linjie, Zhang Jiaming, et al. Evidences of the Late Paleozoic Extensional Setting of the Eastern Central Asian Orogenic Belt:Sedimentological and Chronological Studies of the Zhesi Formation in Shuangjing Area,Inner Mongolia[J]. Acta Petrologica Sinica, 2018, 34(10):3052-3070.
[13] Khain E V, Bibikova E V, Salnikova E B, et al. The Palaeo-Asian Ocean in the Neoproterozoic and Early Palaeozoic:Newgeochronologic Data and Palaeotectonic Reconstructions[J]. Precambrian Research, 2003, 122(1/2/3/4):329-358.
[14] Xu B, Charvet J, Chen Y, et al. Middle Paleozoic Convergent Orogenic Belts in Western Inner Mongolia (China):Framework, Kinematics, Geochronology and Implications for Tectonic Evolution of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013, 23(4):1342-1364.
[15] 邵济安,王友,唐克东.有关内蒙古西拉木伦带古生代-早中生代构造环境的讨论[J].岩石学报,2017, 33(10):3002-3010. Shao Ji'an, Wang You,Tang Kedong. A Reflection on the Xarmoron Tectonomagmatic Belt, Inner Mongolia, China[J]. Acta Petrologica Sinica, 2017, 33(10):3002-3010.
[16] 徐备,赵盼,鲍庆中,等.兴蒙造山带前中生代构造单元划分初探[J].岩石学报,2014,30(7):1841-1857. Xu Bei, Zhao Pan, Bao Qingzhong, et al. Preliminary Study on the Pre-Mesozoic Ttectonic Unit Division of the Xing-Meng Orogenic Belt (XMOB)[J]. Acta Petrologica Sinica, 2014, 30(7):1841-1857.
[17] Liu Y J, Li W M.A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt[J]. Gondwana Research, 2017, 43:123-148.
[18] 周建波,石爱国,景妍. 东北地块群:构造演化与古大陆重建[J].吉林大学学报(地球科学版),2016, 46(4):1042-1055. Zhou Jianbo, Shi Aiguo, Jing Yan. The Combined NE China Blocks:Tectonic Evolution and Super Continent Reconstrucions[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(4):1042-1055.
[19] Anderson T. Correction of Common Lead in U-Pb Analyses that Do Not Report 204Pb[J]. Chemical Geology, 2003, 192:59-79.
[20] Yang J H, Wu F Y, Wilde S A, et al. Petrogenesis and Geodynamics of Late Archean Magmatism in Eastern Hebei, Eastern North China Craton:Geochronological,Geochemical and Nd-Hf Isotopic Evidence[J]. Precambrian Research, 2008, 167:125-149.
[21] Zhu Y F, Sun S H, Gu L B, et al. Permian Volcanism in the Mongolian Orogenic Zone, Ortheast China:Geochemistry, Magma Sources and Petrogenesis[J]. Geological Magazine, 2001, 138(2):101-115.
[22] Zhang X H, Zhang H F, Tang Y J, et al. Geochemistry of Permian Bimodal Volcanic Rocks from Central Inner Mongolia, North China:Implication for Tectonic Setting and Phanerozoic Continental Growth in Central Asian Orogenic Belt[J]. Chemical Geology, 2008, 249(3):262-281.
[23] 程天赦,杨文静,王登红.内蒙古锡林浩特毛登牧场大石寨组细碧-角斑岩系地球化学特征、锆石U-Pb年龄及地质意义[J].现代地质,2013, 27(3):525-536. Cheng Tianshe, Yang Wenjing, Wang Denghong. Zircon U-Pb Age of the Spilite-Keratophyre Sequence of the Dashizhai Formation in Maodeng of Xilinhaote,Inner, Mongolia and Its Geological Significance[J]. Geoscience, 2013, 27(3):525-536.
[24] 晨辰, 张志诚, 郭召杰, 等.内蒙古达茂旗满都拉地区早二叠世基性岩的年代学, 地球化学及其地质意义[J]. 中国科学:地球科学,2012, 42(3):343-358. Chen Chen, Zhang Zhicheng, Guo Zhaojie, et al. Geochronology, Geochemistry, and Its Geological Significance of the Permian Mandula Mafic Rocks in Damaoqi, Inner Mongolia[J]. Science China:Earth Sciences, 2012, 55:39-52.
[25] 梅可辰,李秋根,王宗起,等.内蒙古中部苏尼特左旗大石寨组流纹岩SHRIMP锆石U-Pb年龄、地球化学特征及其构造意义[J]. 地质通报,2015, 34(12):2181-2194. Mei Kechen, Li Qiugen, Wang Zongqi, et al. SHRIMP Zircon U-Pb Age,Geochemistry and Tectonic Significance of the Dashizhai Formation Rhyolites in Sunid Left Banner, Middle Part of Inner Mongolia[J]. Geological Bulletin of China, 2015, 34(12):2181-2194.
[26] 张晓飞,刘俊来,冯俊岭,等.内蒙古锡林浩特乌拉苏太大石寨组火山岩年代学、地球化学特征及其地质意义[J].地质通报,2016, 35(5):766-775. Zhang Xiaofei, Liu Junlai, Feng Junling,et al. Geochronological and Geochemical Features of Volcanic Rocks of Dashizhai Formation in Ural Sutai of Xilin Hot, Inner Mongolia, and Their Geological Significance[J]. Geological Bulletin of China, 2016, 35(5):766-775.
[27] 关庆彬,刘正宏,白新会,等.内蒙古巴林右旗新开坝地区大石寨组火山岩形成时代及构造背景[J]. 岩石学报,2016, 32(7):2029-2040. Guan Qingbin, Liu Zhenghong, Bai Xinhui, et al. Age and Tectonic Setting of Volcanic Rocks of the Dashizhai Formation from Xinkaiba,Balinyouqi Area,Inner Mongolia[J]. Acta Petrologica Sinica, 2016, 32(7):2029-2040.
[28] 蒋干清,张维杰,肖荣阁,等.内蒙古苏尼特左旗地区二叠纪地层的划分与对比[J]. 现代地质,1995, 9(2):149-161. Jiang Ganqing, Zhang Weijie, Xiao Rongge, et al. Subdivision and Correlation of Permian Strataion Sonid Zuoqi Area,Inner Mongolia[J]. Geosciences, 1995, 9(2):149-161.
[29] 刘建峰,迟效国,张兴洲,等. 内蒙古西乌旗南部石炭纪石英闪长岩地球化学特征及其构造意义[J].地质学报, 2009, 83(3):365-376. Liu Jianfeng, Chi Xiaoguo, Zhang Xingzhou, et al. Geochemical Characteristic of Carboniferous Quartz Diorite in the Southern Xiwuqi Area, Inner Mongolia and Its Tectonic Significance[J]. Acta Geologica Sinica, 2009, 83(3):365-376.
[30] 施光海,刘敦一,张福勤, 等.中国内蒙古锡林郭勒杂岩SHRIMP锆石U-Pb年代学及意义[J].科学通报, 2003, 48(20):2187-2192. Shi Guanghai, Liu Dunyi, Zhang Fuqin,et al. Ziron SHRIMP U-Pb Geochronology and Significance of the Xilinhot Metamorphic Complex, Inner Mongolia,China[J]. Chinese Science Bulletin, 2003, 48(20):2187-2192.
[31] 辛后田, 滕学建, 程银行.内蒙古东乌旗宝力高庙组地层划分及其同位素年代学研究[J]. 地质调查与研究, 2011, 34(1):1-9. Xin Houtian, Teng Xuejian, Cheng Yinhang. Stratigraphic Subdivision and Isotope Geochronology Study on the Baoligaomiao Formation in the East Ujimqin County, Inner Mongolia[J]. Geological Survey and Research, 2011, 34(1):1-9.
[32] 潘世语, 迟效国, 孙巍, 等. 内蒙古苏尼特右旗晚石炭世本巴图组火山岩地球化学特征及构造意义[J]. 世界地质, 2012, 31(1):40-50. Pan Shiyu, Chi Xiaoguo, Sun Wei, et al. Geochemical Characteristics and Tectonic Significance of Late Carboniferous Volcanic Rocks in Benbatu Formation of Sonid Youqi,Inner Mongolia[J]. Global Geology, 2012, 31(1):40-50.
[33] 刘敦一, 简平, 张旗, 等. 内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据[J]. 地质学报, 2003, 77(3):318-327. Liu Dunyi, Jian Ping, Zhang Qi, et al. Shrimp Dating of Adakites in the Tulinkai Ophiolite,Inner Mongolia:Evidence for the Early Paleozoic Subduction[J]. Acta Geologica Sinica, 2003, 77(3):318-327.
[34] Jian P, Liu D Y, 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, 101:233-259.
[35] Miao L C, Zhang F Q, Fan W M, et al. Phanerozoic Evolution of the Inner Mongolia-Daxinganling Orogenic Belt in North China:Constraints from Geochronology of Ophiolites and Associated Formations[J]. Geological Society, London, Special Publications, 2007, 280:223-237.
[36] 石玉若, 刘敦一, 张旗, 等. 内蒙古苏左旗地区闪长-花岗岩类SHRIMP年代学[J]. 地质学报, 2004, 78(6):789-799. Shi Yuruo, Liu Dunyi, Zhang Qi,et al. SHRIMP Dating of Diorites and Granites in Southern Suzuoqi,Inner Mongolia[J]. Acta Geologica Sinica, 2004, 78(6):789-799.
[37] Chen B, Jahn B M, Wilde S, et al. Two Contrasting Paleozoic Magmatic Belts in Northern Inner Mongolia,China:Petrogenesis and Tectonic Implications[J]. Tectonophysics, 2000, 328(1/2):157-182.
[38] 薛怀民,郭利军,侯增谦,等.中亚造山带东段的锡林郭勒杂岩:早华力西造山作用的产物而非古老地块锆石SHRIMP U-Pb年代学证据[J].岩石学报,2010, 25(8):2001-2010. Xue Huaimin, Guo Lijun, Hou Zengqian, et al. The Xilinguole Complex from the Eastern Part of the Central Asian-Mongolia Orogenic Belt, China:Products of Early Variscan Orogeny Other than Ancient Block:Evidence from Zircon SHRIMP U-Pb Ages[J]. Acta Petrologica Sinica, 2010, 25(8):2001-2010.
[39] 裴福萍,许文良,杨德彬,等.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义[J].科学通报, 2006, 51(24):2881-2887. Pei Fuping, Xu Wenliang, Yang Debin, et al. Zircon U-Pb Geochronology for Metamorphic Rocks from Basement of the Songliao Basin and Its Geological Implication[J]. Chinese Science Bulletin, 2006, 51(24):2881-2887.
[40] Tang K D. Tectonic Development of Paleozoic Foldbelts at the North Margin of the Sino-Korean Craton[J]. Tectonics, 1990, 9(2):249-260.
[41] 赵一鸣, 毕承思, 邹晓秋, 等. 黑龙江多宝山、铜山大型斑岩铜(钼)矿床中辉钼矿的铼-锇同位素年龄[J]. 地球学报, 1997, 18(1):61-67. Zhao Yiming, Bi Chengsi, Zou Xiaoqiu, et al. The Re-Os Isotopic Age of Molybdenite from Duobaoshan and Tongshan Porphyry Copper (Molybdenum) Deposits[J]. Acta Geoscientica Sinica, 1997, 18(1):61-67.
[42] 武广, 孙丰月, 赵财胜.额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义[J]. 科学通报,2005, 50(20):2733-2743. Wu Guang, Sun Fengyue, Zhao Caisheng. Discovery of the Early Paleozoic Post-Collisional Granites in the Northern Margin of the Erguana Massif and Its Geological Significance[J]. Chinese Science Bulletin, 2005, 50(20):2733-2743.
[43] 葛文春,隋振民,吴福元, 等.大兴安岭东北部早古生代花岗岩错石U-Pb年龄、Hf同位素特征及地质意义[J].岩石学报, 2007, 23(2):423-440. Ge Wenchun, Sui Zhenmin, Wu Fuyuan, et al. Zircon U-Pb Ages,Hf Isotopic Characteristics and Their Implications of the Early Paleozoic Granites in the Northeastern Da Hinggan Mts,Northeastern China[J]. Acta Petrologica Sinica, 2007, 23(2):423-440.
[44] 周建波,张兴洲,Wilde S A,等.中国东北~500Ma泛非期孔兹岩带的确定及其意义[J]. 岩石学报,2011, 27(4):1235-1245. Zhou Jianbo, Zhang Xingzhou, Wilde S A, et al. Confirming of the Heilongjiang~500Ma Pan-African Khondalite Belt and Its Tectonic Implications[J]. Acta Petrologica Sinica, 2011, 27(4):1235-1245.
[45] Miao L C, Liu D Y, Zhang F Q, et al. Zircon SHRIMP U-Pb Ages of the Xinghuadukou Group in Hanjiayuanzi and Xinlin Areas and the Zhalantun Group in Inner Mongolia, Da Hinggan Mountains[J]. Chinese Science Bulletin, 2007, 52(5):591-601.
[46] Zhou J B, Wilde S A, Zhang X Z, et al. Pan-African Metamorphic Rocks of the Erguna Massif in the Great Xing'an Range, NE China:Evidence and Tectonic Implications[J]. Tectonophysics, 2011, 499(1/2/3/4):105-117.
[47] Guo J H, Sun M, Chen F K, et al. Sm-Nd and SHRIMP U-Pb Zircon Geochronology of High-Pressure Granulites in the Sanggan Area, North China Craton:Timing of Paleoproterozoic Continental Collision[J]. Journal of Asian Earth Sciences, 2005, 24:629-642.
[48] 郭晓丹, 周建波, 张兴洲, 等.内蒙古西乌珠穆沁旗本巴图组碎屑锆石LA-ICP-MS U-Pb年龄及其意义[J]. 地质通报, 2011, 30(2/3):278-290. Guo Xiaodan, Zhou Jianbo, Zhang Xingzhou, et al. The Detrital Zircon LA-ICP-MS U-Pb Ages and Its Significance of Benbatu for Mation in Xiwuzhu Muqinqi, Inner Mongolia, China[J]. Geological Bulletin of China, 2011, 30(2/3):278-290.
[49] 宋卫卫, 周建波, 郭晓丹, 等. 松辽地块大地构造属性:古生界碎屑锆石年代学的制约[J]. 世界地质, 2012, 31(3):522-535. Song Weiwei, Zhou Jianbo, Guo Xiaodan, et al. Geotectonic Setting of Songliao Block:Reatriction from Paleozoic Detrital Zircon U-Pb Dating[J]. Global Geology, 2012, 31(3):522-535.
[50] 郑月娟,张海华,陈树旺,等. 内蒙古阿鲁科尔沁旗林西组砂岩LA-ICP-MS锆石U-Pb年龄及意义[J]. 地质通报,2014, 33(9):1293-1307. Zheng Yuejuan, Zhang Haihua, Chen Shuwang, et al. LA-ICP-MS U-Pb Age of Detrital Zircons from Late Permian Linxi Formation in Ar Horqin Banner,Inner Mongolia[J]. Geological Bulletin of China, 2014, 33(9):1293-1307.
[51] 隋振民,葛文春,徐学纯,等. 大兴安岭十二站晚古生代后造山花岗岩的特征及其地质意义[J]. 岩石学报,2009, 25(10):2679-2686. Sui Zhenmin, Ge Wenchun, Xu Xuechun, et al. Characteristics and Geological Implications of the Late Paleozoic Post Orogenic Shierzhan Granite in the Great Xing'an Range[J]. Acta Petrologica Sinica, 2009, 25(10):2679-2686.
[52] 李鹏川,刘正宏,李世超,等. 内蒙古巴林右旗胡都格绍荣岩体的年代学、地球化学、Hf同位素特征及构造背景[J]. 地球科学,2016, 41(12):1995-2007. Li Pengchuan, Liu Zhenghong, Li Shichao, et al. Geochronolgy, Geochemistry, Zircon Hf Isotopic Characteristics and Tectonic Setting of Hudugeshaorong Pluton in Balinyouqi,Inner Mongolia[J]. Earth Science, 2016, 41(12):1995-2007.
[53] Kelty T K,Yin A, Dash B, et al. Detrital Zircon Geochronology of Paleozoic Sedimentary Rock in the Hangay-Hentey Basin, Northcentral Mongolia:Implications for the Tectonic Evolution of the Mongol-Okhotsk Ocean in Central Asia[J].Tectonophysics, 2008, 451:97-122.
[54] 栗进,徐备,田英杰,等.内蒙古克什克腾旗哲斯组沉积学和年代学研究及其古地理意义[J]. 岩石学报,2018, 34(10):3034-3050. Li Jin, Xu Bei, Tian Yingjie, et al. Sedimentary and Geochronology Study on the Zhesi Formation from Hexigten Banner,Inner Mongolia and Paleogeographic Significances[J]. Acta Petrologica Sinica, 2018, 34(10):3034-3050.
[55] 朱俊宾,和政军. 内蒙古林西地区上二叠统-中三叠统沉积序列的碎屑锆石记录及对古亚洲洋(东段)闭合时间的制约[J].地质学报,2017, 91(1):232-248. Zhu Junbin, He Zhengjun. Detrital Zircon Records of Upper Permian-Middle Triassic Sedimentary Sequence in the Linxi Area,Inner Mongolia and Constraints on Timing of Final Closure of the Paleo-Asian Ocean(Eastern Segment)[J]. Acta Geologica Sinica, 2017, 91(1):232-248.
[56] 钱程, 陈会军,陆露,等. 黑龙江省龙江地区新太古代花岗岩的发现[J]. 地球学报,2018, 39(1):27-36. Qian Cheng, Chen Huijun, Lu Lu, et al. The Discovery of Neoarchean Granite in Longjiang Area, Heilongjiang Province[J]. Acta Geoscientica Sinica, 2018, 39(1):27-36.
[57] 孙立新, 任邦方, 赵凤清,等. 内蒙古额尔古纳地块古元古代末期的岩浆记录:来自花岗片麻岩的锆石U-Pb年龄证据[J]. 地质通报, 2013, 32(2/3):341-352. Sun Lixin, Ren Bangfang, Zhao Fengqing, et al. Late Paleoproterozoic Magmatic Rrecords in the Eerguna Massif:Evidences from the Zircon U-Pb Dating of Granitic Gneisses[J]. Geological Bulletin of China, 2013, 32(2/3):341-352.
[58] 邵军, 李永飞, 周永恒, 等. 中国东北额尔古纳地块新太古代岩浆事件:钻孔片麻状二长花岗岩锆石LA-ICP-MS测年证据[J]. 吉林大学学报(地球科学版),2015, 45(2):364-373. Shao Jun, Li Yongfei, Zhou Yongheng, et al. Neo-Archean Magmatic Event in Erguna Massif of Northeast China:Evidence from the Zircon LA-ICP-MS Dating of the Geneissic Monzogranite from the Drill[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(2):364-373.
[59] 吴才来, 陈安泽, 高前明,等. 东北伊春地区桃山古元古代花岗岩的发现[J]. 地质学报,2010, 84(9):1324-1332. Wu Cailai, Chen Anze, Gao Qianming, et al. Discovery of the Paleo-Proterozoic Granite in Taoshan, Yichun, Northeastern China[J]. Acta Geologica Sinica, 2010, 84(9):1324-1332.
[60] Fleet A R. Aqueous and Sedimentary Geochemistry of the Race Earth Elements[M]//Henderson P. Rare Earth Element Geochemistry.[S.L.]:Elsevier, 1984:331-373.
[61] Mclennan S M. Rare Earth Elements in Sedimentary Rocks:Influence of Provenance and Sedimentary Rocesses[J]. Reviews in Mineralogy, 1989, 21:169-200.
[62] 任纪舜,牛宝贵,刘志刚. 软碰撞、叠覆造山和多旋回缝合作用[J]. 地学前缘,1999, 6(3):85-93. Ren Jishun, Niu Baogui, Liu Zhigang. Soft Collision,Superposition Orogeny and Polycyclic Suturing[J]. Earth Science Frontiers, 1999, 6(3):85-93.
[63] 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):339-352. 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
[64] Zhou J B,Cao J L,Wilde S A,et al. Paleo-Pacific Subduction-Accretion:Evidence from Geochemical and U-Pb Zircon Dating of the Nadanhada Accretionary Complex,NE China[J]. Tectonics, 2014, 33(12):2444-2466.
[65] 张兴洲,马玉霞,迟效国,等.东北及内蒙古东部地区显生宙构造演化的有关问题[J]. 吉林大学学报(地球科学版),2012, 42(5):1269-1285. Zhang Xingzhou,Ma Yuxia,Chi Xiaoguo,et al. Discussion on Phanerozoic Tectonic Evolution in Northastern China[J].Journal of Jilin University(Earth Science Edition), 2012, 42(5):1269-1285.
[66] 王成文, 金巍, 张兴洲, 等.东北及邻区晚古生代大地构造属性新认识[J].地层学杂志,2008, 32(2):1269-1285. Wang Chengwen, Jin Wei, Zhang Xingzhou, et al. New Understanding of the Late Paleozoic Tectonics in Northeastern China and Adjacent Areas[J]. Journal of Stratigraphy, 2008, 32(2):1269-1285.
[67] 赵芝, 迟效国, 潘世语,等. 小兴安岭西北部石炭纪地层火山岩的锆石LA-ICP-MS U-Pb年代学及其地质意义[J]. 岩石学报, 2010, 26(8):2452-2464. Zhao Zhi,Chi Xiaoguo,Pan Shiyu,et al. Zircon U-Pb LA-ICP-MS Dating of Carboniferous Volcanics and Its Geological Significance in the Northwestern Lesser Xing'an Range[J]. Acta Petrologica Sinica,2010, 26(8):2452-2464.
[68] Tang K D. Tectonic Development of Paleozoic Fold Belts at the North Margin of the Sino-Korean Craton[J]. Tectonics, 1990(9):249-260.
[69] 吕志成, 郝立波, 段国正,等. 大兴安岭南段早二叠世两类火山岩岩石地球化学特征及其构造意义[J]. 地球化学,2002, 31(4):338-346. Lü Zhicheng, Hao Libo, Duan Guozheng, et al. Lithogeochemical Characteristics and Tectonic Implications of Two Series of Volcanic Rocks from Early Permian Dashizhai Formation in the South Section of Da Hinggan Mountains[J]. Geochimica, 2002, 31(4):338-346.
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