吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (5): 1418-1429.doi: 10.13278/j.cnki.jjuese.201605112

• 地质与资源 • 上一篇    下一篇

吉林中部小蜂蜜顶子组火山岩的形成时代及其地质意义:锆石U-Pb年代学和Hf同位素组成证据

张海洪1,2, 许文良1, 王枫1, 曹花花1,3   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林省地质调查院, 长春 130021;
    3. 中国海洋大学海洋地球科学学院, 山东 青岛 266100
  • 收稿日期:2015-12-07 出版日期:2016-09-26 发布日期:2016-09-26
  • 通讯作者: 许文良(1959-),男,教授,博士生导师,主要从事火成岩石学和岩石圈动力学方面研究,E-mail:xuwl@jlu.edu.cn E-mail:xuwl@jlu.edu.cn
  • 作者简介:张海洪(1986-),男,博士研究生,工程师,主要从事岩石地球化学方面研究,E-mail:seaflood@163.com
  • 基金资助:

    国家自然科学基金项目（41072038）；中国地质调查局项目（12120113098300）

Formation Timing of the Volcanic Rocks from the Xiaofengmidingzi Formation in Central Jilin Province and Its Geological Implications: Evidence from Zircon U-Pb Dating and Hf Isotope Compositions

Zhang Haihong1,2, Xu Wenliang1, Wang Feng1, Cao Huahua1,3   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Institute of Geologic Survey, Jilin Province, Changchun 130021, China;
    3. College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China
  • Received:2015-12-07 Online:2016-09-26 Published:2016-09-26
  • Supported by:

    Supported by the National Natural Science Foundation of China Project (41072038) and China Geological Survey's Program Project (12120113098300)

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265

摘要：

本文对出露于吉林省中部地区的小蜂蜜顶子组标准剖面的流纹岩（样品号：JH21-1）和非标准剖面小蜂蜜顶子组的安山岩（样品号：JX1-1）进行了锆石LA-ICP-MS U-Pb年代学以及Hf同位素组成研究。2个样品中的锆石均呈自形-半自形，CL图像上显示条痕状吸收或典型的岩浆振荡生长环带，结合其Th/U比值（0.27~0.81），均暗示了它们的岩浆成因。定年结果表明：流纹岩（JH21-1）中锆石206Pb/238U加权平均年龄为（192±2）Ma （MSWD=4.8），其形成于早侏罗世；安山岩（JX1-1）中锆石206Pb/238U加权平均年龄为（172±1）Ma （MSWD=0.27），表明其形成于中侏罗世。前者与标准剖面时代一致，后者与小蜂蜜顶子组并非同一套火山岩。而2个样品中锆石的Hf同位素组成较为均一，εHf（t）值为+5.25~+9.37，二阶省模式年龄为803~1 177 Ma，暗示它们起源于中-新元古代新增生陆壳物质的部分熔融。综上所述，吉林中部地区侏罗纪岩浆事件至少可以划分为两期——早侏罗世和中侏罗世，结合区域构造演化历史，可以认为吉林省中部地区早-中侏罗世火山岩的形成应与古太平洋板块俯冲于欧亚大陆之下的地质作用相联系。

关键词: 吉林中部, 小蜂蜜顶子组, 火山岩, 锆石U-Pb年代学, 岩石组合, 构造意义

Abstract:

The data of LA-ICP-MS zircon U-Pb dating and Hf isotopes are reported for the rhyolite (JH21-1) from typical section and the andesite (JX1-1) from another section of the Xiaofengmidingzi Formation in the central Jilin Province, NE China. The zircons from two volcanic rocks are euhedral-subhedral in shape and display striped absorption or oscillatory growth zoning in the CL images, and have high Th/U ratios (0.27-0.81), implying their magmatic origin. The dating results indicate that the zircons from the rhyolite (JH21-1) yield a weighted mean 206Pb/238U age of (192±2) Ma (MSWD=4.8), i.e., the Early Jurassic, and the zircons from the andesite (JX1-1) yield a weighted mean 206Pb/238U age of (172±1) Ma (MSWD=0.27), i.e., the Middle Jurassic. The former is consistent with the timing of the typical section, and the latter is different from the typical Xiaofengmidingzi Formation. Their zircon εHf(t) (172-192 Ma) values range from +5.25 to +9.37, and Hf two-stage model ages vary from 803 Ma to 1 177 Ma,implying that their primary magmas were derived from partial melting of the juvenile lower crust. Taken together, it is suggested that the Jurassic magmatism can be subdivided into two stages, i.e., the Early Jurassic and Middle Jurassic. Combined with regional tectonic evolution history, we conclude that the Jurassic magmatism in the central Jilin Province could be related to the subduction of the Paleo-Pacific plate beneath the Eurasian continent.

Key words: central Jilin Province, Xiaofengmidingzi Formation, volcanic rocks, zircon U-Pb chronology, rock association, tectonic implication

中图分类号: 

  • P588.14

[1] Sengör A M C, Natal'in B A, Burtman V S. Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia[J]. Nature, 1993, 364:299-307.

[2] Sengör A M C, Natal'in B A. Paleotectonics of Asia:Fragments of a Synthesis[C]//Yin A, Harrison M. The Tectonic Evolution of Asia. London:Cambridge University Press, 1996:486-640.

[3] 李锦轶.中国东北及邻区若干地质构造问题的新认识[J]. 地质评论,1998, 44(4):310-347. Li Jinyi. Some New Ideas on Tectonics of NE China and Its Neighboring Areas[J]. Geological Review, 1998, 44(4):310-347.

[4] Wu F Y, Sun D Y, Li H M, et al. A-Type Granites in Northeastern China:Age and Geochemical Constraints on Their Petrogenesis[J]. Chemical Geology, 2002, 187(1/2):143-173.

[5] Wu F Y, Yang J H, Lo C H, et al. The Heilongjiang Group:A Jurassic Accretionary Complex in the Jiamusi Massif at the Western Pacific Margin of Northeastern China[J]. The Island Arc, 2007, 16(1):156-172.

[6] Li J Y. Permian Geodynamic Setting of Northeast China and Adjacent Regions:Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26:207-224.

[7] Xu W L, Ji W Q, Pei F P, 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.

[8] Wang F, Xu W L, Gao F H, et al. Tectonic History of the Zhangguangcailing Group in Eastern Heilongjiang Province,NE China:Constraints from U-Pb Geochronology of Detrital and Magmatic Zircons[J]. Tectonophysics, 2012(566/567):105-122.

[9] Wang F, Xu W L, Meng E, et al. Early Paleozoic Amal-gamation of the Songnen-Zhangguangcai Range and Jiamusi Massifs in the Eastern Segment of the Central Asian Orogenic Belt:Geochronological and Geochemical Evidence from Granitoids and Rhyolites[J]. Journal of Asian Earth Sciences, 2012, 49:234-248.

[10] 裴福萍,许文良,杨德彬,等. 松辽盆地南部中生代火山岩:锆石U-Pb年代学及其对基底性质的制约[J].地球科学:中国地质大学学报, 2008, 33(5):603-617. Pei Fuping, Xu Wenliang, Yang Debin, et al. Mesozoic Volcanic Rocks in the Southern Songliao Basin:Zircon U-Pb Ages and Their Constraints on the Nature of Basin Basement[J]. Earth Science:Journal of China University of Geology, 2008, 33(5):603-617.

[11] 赵越,杨振宇,马醒华.东亚大地构造发展的重要转折[J].地质科学,1994,29(2):105-114. Zhao Yue, Yang Zhenyu, Ma Xinghua. Geotectonic Transition from Paleo Asian System and Paleotethyan System to Paleopacific Active Continental Margin in Eastern Asia[J]. Scientia Geologica Sinica, 1994, 29(2):105-114.

[12] 彭玉鲸,王友勤,刘国良,等.吉林省及东北部邻区的三叠系[J].吉林地质,1982,3:1-19. Peng Yujing, Wang Youqin, Liu Guoliang, et al. The Triassic System of Jilin Province and Its Northeastern Adjacent Areas[J]. Jilin Geology, 1982, 3:1-19.

[13] 彭玉鲸,陈跃军.吉黑造山带与华北地台开原-山城镇段构造边界位置[J].世界地质,2007, 26(1):1-6. Peng Yujing, Chen Yuejun. Location of Structural Boundary Between Ji-Hei Orogenic Zone and Kaiyuan-Shancheng Town Section of North China Platform[J]. Global Geology, 2007, 26(1):1-6.

[14] 王五力.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. The Evolution and Transformation of Paleo-Asia and Paleo-Pacific Tectonic Domain of Northeast China[J]. Geology and Resources, 2012, 21(1):27-34.

[15] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30.

[16] 吉林省地质矿产局.中华人民共和国区域地质调查报告(1:20万):长春市幅K-51-Ⅵ[M].北京:地质出版社, 1978. Jilin Bureau of Geology and Mineral Resources. Report of the Regional Geological Survey of the People's Republic of China (1:200000):Changchun Mapping Project K-51-Ⅵ[M]. Beijing:Geological Publishing House, 1978.

[17] 吉林省地质矿产局.中华人民共和国区域地质调查报告(1:20万):吉林市幅K-52-(1)[M].北京:地质出版社,1970. Jilin Bureau of Geology and Mineral Resources. Report of the Regional Geological Survey of the People's Republic of China (1:200000):Jilin Mapping Project K-52-(1)[M]. Beijing:Geological Publishing House, 1970.

[18] Zhang Y B, Wu F Y, Wilde S A, et al. Zircon U-Pb Ages and Tectonic Implications of "Early Paleozoic" Granitoids at Yanbian, Jilin Province, NE China[J]. The Island Arc, 2004, 13:484-505.

[19] 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. Jilin Bureau of Geology and Mineral Resources. Regional Geology of Jilin Province[M]. Beijing:Geological Publishing House, 1988.

[20] Yuan H L, Gao S, Liu X M, et al. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation Inductively Coupled Plasma Mass Spectrometry[J]. Geostandard Newsletter:The Journal of Geostandards and Geoanalysis, 2004, 28:353-370.

[21] Liu Y S, Gao S, Hu Z C, et al. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths[J]. Journal of Petrology, 2009, 51(1/2):537-571.

[22] Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546.

[23] Black L P, Kamo S L, Allen C M, et al. TEMORA 1:A New Zircon Standard for Phanerozoic U-Pb Geochronology[J]. Chemical Geology, 2003, 200(1/2):155-170.

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

[25] Ludwig K R. Using Isoplot/EX, Version 2. 49. A Geochronological Toolkit for Microsoft Excel[M]. Berkeley:Berkeley Geochronological Center Special Publication, 2001:1-55.

[26] Xu P, Wu F Y, Xie L W, et al. Hf Isotopic Composi-tions of the Standard Zircons for U-Pb Dating[J]. Chinese Science Bulletin, 2004, 49(15):1642-1648.

[27] Wu F Y, Yang Y H, Xie L W, et al. Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology[J]. Chemical Geology, 2006, 234(1/2):105-126.

[28] Koschek G. Origin and Significance of the SEM Catho-doluminescence from Zircon[J]. Journal of Microscopy, 1993, 171:223-232.

[29] Yang J H, Wu F Y, Shao J, et al. Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt, North China[J]. Earth and Planetary Science Letters, 2006, 246:245-336.

[30] 吉林省地质矿产局.中华人民共和国区域地质调查报告(1:20万):舒兰市幅K-51-ⅩⅩⅩⅠ[M].北京:地质出版社,1980. Jilin Bureau of Geology and Mineral Resources. Report of the Regional Geological Survey of the People's Republic of China (1:200000):Sulan Mapping Project K-51-ⅩⅩⅩⅠ[M]. Beijing:Geological Publishing House, 1980.

[31] 王光奇,于宏斌,宋成印,等.土们岭-八台岭-马大山晚二叠世"马达屯组"的时代及特征讨论[J].吉林地质,1988, 17(4):11-19. Wang Guangqi, Yu Hongbin, Song Chengyin, et al. The Age of the Late Permian "Madatun Formation" in the Tumenling-Batailing-Madashan and Its Charac-teristics[J]. Jilin Geology,1988,17(4):11-19.

[32] 武要红,宋竹琴.双阳盆地小蜂蜜顶子组时代的讨论[J].东北煤炭技术,1997,2(1):53-56. Wu Yaohong, Song Zuqin. Discussion on Age of Xiaofengmidingzi Formation in Shuangyang Basin[J]. Coal Technology of Northeast China, 1997,2(1):53-56.

[33] 孙德有,吴福元,高山,等.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J]. 地学前缘,2005,12(2):263-275. Sun Deyou, Wu Fuyuan, Gao Shan, et al. Confirmation of Two Episodes of A-Type Granite Emplacement During Late Triassic and Early Jurassic in the Central Jilin Province and Their Constraints on the Structural Pattern of the East Jilin-Heilongjiang Area, China[J]. Earth Science Frontiers, 2005, 12(2):263-275.

[34] 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 Process in Northern Margin of North China Craton During Synergic Process of Paleo-Asian Ocean and Paleo-Pacific Plate[J]. Science in China:Series D, 1997, 27(5):390-394.

[35] 邵济安,张履桥, 牟保磊, 等.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, Mu Baolei, et al. Magmatism in the Mesozoic Extending Orogenic Process of Da Hinggan Mts[J]. Earth Science Frontiers, 1999, 6(4):339-346.

[36] 李益龙,周汉文,肖文交,等.古亚洲构造域和西太平洋构造域在索伦缝合带东段的叠加:来自内蒙古林西县西拉木伦断裂带内变形闪长岩的岩石学、地球化学和年代学证据[J]. 地球科学:中国地质大学学报,2012,37(3):433-450. Li Yilong, Zhou Hanwen, Xiao Wenjiao, et al. Superposition of Paleo-Asian and West-Pacific Tectonic Domains in the Eastern Section of the Solonker Suture Zone:Insights from Petrology, Geochemistry and Geochronology of Deformed Diorite in Xar Moron Fault Zone, Inner Mongolia[J]. Earth Science:Journal of China University of Geosciences, 2012, 37(3):433-450.

[37] 柴田贤, 王松山,胡世玲,等.钾长石的K-Ar年龄和封闭温度[J].地质地球化学,1994, 22(5):44-50. Chai Tianxian, Wang Songshan, Hu Shiling, et al. The K-Ar Dating Age and Closure Temperature of K-Feldspar[J]. Geology-Geochemistry, 1994, 22(5):44-50.

[38] 桑海清.迁安蟒山岩体黑云母的40Ar-39Ar年龄谱及封闭温度[J].岩石学报,1992,8(4):332-340. Sang Haiqing. Closure Temperature and 40Ar-39Ar Age Spectrum of Biotites from Mangshan Granodiorite-Tonalite in Qian' an County, Hebei Province[J]. Acta Petrologica Sinica, 1992, 8(4):332-340.

[39] 刘尔义.张广才岭-南楼山地层分区中、新生代地层[J].吉林地质,1996,15(3/4):89-95. Liu Eryi. Meso-Cenozoic Stratigraphy of Zhangguang-cailing-Nanloushan Stratigraphical Subprovince[J]. Jilin Geology, 1996, 15(3/4):89-95.

[40] 孙罡,杨占军,丁淑燕,等.吉林中部地区南楼山组时代确认[J].吉林地质,2011, 30(3):25-30. Sun Gang, Yang Zhanjun, Ding Shuyan, et al. Time Determination of the Nanloushan Formation in the Central Part of Jilin Province[J]. Jilin Geology, 2011, 30(3):25-30.

[41] 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):286-287. Xu Wenliang, Ge Wenchun, Pei Fuping, et al. Geochronological Frame of Mesozoic Volcanism in NE China and Its Significance[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2008, 27(Sup.):286-287.

[42] 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.

[43] 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.

[44] 徐美君,许文良,王枫,等.小兴安岭西北部早侏罗世花岗质岩石的年代学与地球化学及其构造意义[J].岩石学报,2013,29(2):354-368. Xu Meijun, Xu Wenliang, Wang Feng, et al. Geochronology and Geochemistry of the Early Jurassic Granitoids in the Central Lesser Xing'an Range, NE China and Its Tectonic Implications[J]. Acta Petrologica Sinica, 2013, 29(2):354-368.

[45] Yu J J, Wang F, Xu W L, et al. Early Jurassic Mafic Magmatism in the Lesser Xing'an-Zhangguangcai Range, NE China and Its Tectonic Implications:Constrains from Zircon U-Pb Chronology and Geochemistry[J]. Lithos, 2012, (142/143):256-266.

[46] Yang J H, Wu F Y, Shao J, et al. Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt, North China[J]. Earth and Planetary Science Letters, 2006, 246:245-336.

[47] 邓晋福,莫宣学,罗照华,等.火成岩构造组合与壳幔成矿系统[J]. 地学前缘,1999,6(2):259-270. Deng Jinfu,Mo Xuanxue,Luo Zhaohua, et al. Igneous Petrotectonic Assemblage and Metallogenic System of Crust-Mantle[J]. Earth Science Frontiers, 1999, 6(2):259-270.
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