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地球学报  2008 

华北古陆中、新元古代年代地层框架SHRIMP锆石年龄新依据

DOI: 10.3975/cagsb.2008.03.10

Keywords: 华北占陆,中、新元古界,大红峪组,下马岭组,SHRIMP年龄

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Abstract:

建立中国晚前寒武纪地层的标准剖而,并使其成为国际地层对比的参考标准,一直是中国地质学家的追求.华北蓟县中、新元古代地层一直作为这一标准地层的主要研究剖面,已进行了岩石地层、生物地层、化学地层、磁性地层和层序地层等多学科研究.但是,高质量的同位素年代学研究和以此为基础的年代地层框架的优化一直是华北古陆中、新元古界研究的薄弱环节.长期以来,由于关键层位和关键界而缺乏高质量的同位素年龄标定,致使蓟县剖面争取成为国际层面标准剖面的竞争力受到影响.近期,随着锆石SHRIMP年龄测定技术在华北古陆前寒武纪地层学研究中的成功应用,在几个关键层位定年研究中取得实质性进展.北京西山下马岭组中部班脱凝灰岩中获得锆石SHRIMP加权平均年龄为(1370±11)Ma,使得下马岭组这个青白口群的关键地层单位划归为中元古界.天津蓟县大红峪组碱性火山岩中获得锆石SHRIMP加权平均年龄为(1625.9±8.9)Ma.可用于标定华北古陆中元古代裂解时间得北京密云环斑花岗岩获得锆石SHRIMP加权平均年龄为(1685±15)Ma.这些SHRIMP测年结果使华北古陆中、新元古界年代地层划分与全球对比有了年龄"锚点",必定有利于准确厘定华北地区中、新元古界的内涵.由于华北蓟县中、新元占界剖面是我国晚前寒武纪地层的标准剖面,因此上述年代地层框架的优化对于我国地质填图的修正和精确地层对比有着重要的促进作用.同时,对于我国前寒武纪生物演化,特别是宏观藻类发育的时间研究具有重要意义.这必定有助于提升华北中、新元古界剖面的国际地位.

References

[1]  GAO Linzhi;QIAO Xiufu,Sinian System,北京:地质出版社,2005.
[2]  GAO Linzh;DING Xiaozhong;YIN Chongyu.Meso and Neoprot-erozoic stmtigraphic sequences in the Southern Ural area and discovery of molar-tooth strctures in carbonate and elastic rocks of the sequences and their geological significance[J].Geology in China,2007(06)
[3]  YIN Chongyu,New U-Pb zircon ages from the Sinian System in the Yangtze Gorges:constraint on the minimum age of the Miaohe biota and Marinoan glaciation,Acta Micropalaeontologica Sinica,2005(zk).
[4]  YIN Changyu,Advance and tendence of the Neoproterozoic chronestratigraphic studies,Journal of Stratigraphy,2005(02).
[5]  WANG Honggzhen;ZHANG Shihong.Tectonic Pattern of the World Precambrian Basement and Problems of Paloocontinent Reconstruction[J].Earth Science-journal of China University of Geosciences,2002(05)
[6]  Vigneresse J L,The specific case of the Mid-Proterozoic rapakivi granites and associated suited with the context of the Columbia Super continent,Precambrian Research? ,2005, 137.
[7]  高林志;丁孝忠;尹崇玉;任留东 李廷栋 陈廷禺 陈柄蔚 李贵书 陆松年.南乌拉尔地区中、新元古代地层序列及碳酸岩和碎屑岩发现臼齿构造的地质意义[J].中国地质,2007(06)
[8]  National Commission on Stratigraphy of China,The minutes of the classification and terminology of late Precambian strate of working meeting,Journal of Stratigraphy,1983(01).
[9]  GRADSTEIN F M;OGG J G;SMITH A G;BLEEKER W,LOURENSL J,A Geologic Time Scale,Cambridge:Cambridge University Press,2004.
[10]  高林志;尹崇玉;王自强.华北地台南缘新元古代地层的新认识[J].地质通报,2002(03)
[11]  万渝生;张巧大;宋天锐.北京十_二陵长城系常州沟组碎屑锆石SHRIMP年龄:华北克拉通盖层物源区及最大沉积年龄的限定[J].科学通报,2003(18)
[12]  高林志;章雨旭;王成述;田树刚, 彭阳, 刘友元, 董大中, 何怀香, 雷宝桐, 陈孟莪, 杨立公,天津蓟县中新元古代层序地层初探,中国区域地质,1996(01).
[13]  XING Ynsheng;Yin Chongyu;Gao Linzhi,The boundary and subdivision of the Sinian System,Geoscience,1999(02).
[14]  XING Yusheng;LIU Guizhi,Late Precambrian microflora of China and its stratigraphical significance,Bulletin of the Chinese Academy of Geological Sciences,1982(04).
[15]  SIN Yusheng;LIU Kuizhih,The Sinian Microflora in Yan-Liaoarea and its geological significance,Acta Geographica Sinica,1973(01).
[16]  XING Yusheng;DUAN Chenghua;LIANG Yuzuo;CAO Renguan,Late Precambrian Paleonology of China.People\' s Republic of China Ministry of Geology and Mineral Resources,geological Memoirs,series(2),number(2),北京:地质出版社,1996.
[17]  XING Yusheng,The Sinian in China,北京:地质出版社,1979.
[18]  XING Ynshang,The upper Precambrian of China.Stratigraphy of China(No.3),北京:地质出版社,1989.
[19]  WANG Ynsheng;ZHANG Qiaeda;SONG Tianrni.Shrimp age of detrital zircons from the Changcheng System in the Ming Tomb Area,Beljing,constraints on the protolith nature and maximum depositional age of the Mesoproterozoic cover of the North China Croton[J].Chinese Science Bulletin,2003(18)
[20]  WANG Hongzhen,On the international stratigraphical chart and stratigraphic ragianalization of China,Genescience,1999(02).
[21]  高振西;熊永先;高甲,中国北部震旦纪地层,中国地质学会会志,1934.
[22]  DENG Jinfu;MO Xuanxue;ZHAO Hailing;LUO Zhaohua, WU Zongxu,Continental Roots[plume].Tectonics of China,北京:地质出版社,1996.
[23]  Derek J. Thorkelson ;J. Grant Abbott ;James K. Mortensen,Early and Middle Proterozoic evolution of Yukon, Canada,Canadian journal of earth sciences?,2005, 42(6).
[24]  SONG Bian;ZHANG Yuhai;WAN Yusheng,Introduction to the Naissance of SHRIMP and its Contribution to Isotope Geology,Geological Review,2002(zk).
[25]  SHATSKY N S,Notes on tectonies of Volga-Ural oil bearing region and adjacent part of the Western slope of the South Ural,Materials to study geological structure of the USSR M,1945(26).
[26]  QIAO Xiufu;GAO Linzhi;ZHANG Chuanheng.New idea of the Meso-and Neoproterozoic ehronoEaratigraphic chart and tectonic environment in Sino-Korean Plate[J].Geological Bulletin of China,2007(05)
[27]  QIAO Xinfu,Investigation on stratigraphy of the Qingbaikou Group of the Yenshan Mountains,North China,Scientia Geologica Sinica,1976.
[28]  OGG J G,Status of divisions of the International Geoloic Time Scale,Lethaia,2004.
[29]  ZHANG Chnanheng;WU Zhenjie;GAO Linzhi;WANG Wei TIAN Yanlin MA Chac,Earthquake-induced soft-sediment deormation structure in the Wnmishan Formation and their geological implications,Science in China(Series D),2008(03).
[30]  LU Songnian;YANG Chunllang;Ll Huaikun;YU Haifeng JIN Wei Guo Kunyi,North China continent and coluumhia Super continent Supercontinent,Earth Sciences Frontiers,2007(04).
[31]  LU Sangnian;LIHnimin,A precise U-Pb singlezircon age deterruination for the volcanies of Dahongyu Foramation,Changeheng System in Jixian,Acta Geoscientica Sinica,1991.
[32]  LIU Yongqing;GAO Linzhi;LIU Yanxue;SONG Bian WANG Zongxiu.Zircon U-Pb dating for the earliest Neopmterozoic mafic magnmtism in the southern margin of the North China Block[J].Chinese Science Bulletin,2008(19)doi:10.1007/s11434-006-2114-0
[33]  LI Huikun;LI Huiming;LU Songnian,Grain zircon U-Pb ages for volcanic rocks from Tuanshanzi formation of Changcheng System and their geological implications,Geochimica,1995(10).
[34]  LANCE P B;SANDBA L K;CHARLO]TE M A;ALEINIKOFF J N DAVIS D W,TEMORA 1:a new zircon standard for Phanerozoic U-Pb geochronology,Chemical Geology,2005.
[35]  高林志;尹崇玉;邢裕盛,新元古代微古植物组合序列与层序地层学,1999.
[36]  Felix M. Gradstein ;James G. Ogg ;Alan G. Smith ;Wouter Bleeker ;Lucas J. Lourens,A New Geologic Time Scale, with special reference to Precambrian and Neogene from the Dabie Mountains, central China,Episodes?,2004, 27(2).
[37]  GENG Ynansheng;YANG Chonghui;DU Lilin;WANG Xinshe BEN Liudong ZHOU Xiwen.Chronology and tectonic environment of the Tianbaeshan Formation:new evidence from zircon SHRIMP U-Pb age and geochemistry[J].Geological Review,2005(04)
[38]  GAO Wei;ZHANG Chnanheng;GAO Linzhi;SHI Xiaoying LIU Yaoming SONG Biao,Zircon SHRIMP U-Pb age of the repakiv granite in Miyun,Beijing and its tectonoestratirphic implication,Geological Bulletin of China,2006(06).
[39]  GAO Linzhi;ZHANG Yuxun;WANG Chengshu;TIAN Shugang PENG Yang LIU Youyuan DONG Dazhong HE Huaixiang CHEN Mang\'e YANC Ligong,Meso-and Neopmterozoic se-quence stratigraphyin Jixian,Regional Geology of China,1996(01).
[40]  GAO Linzhi;ZHANG Chuanheng;SHIi Xiaoying;ZHOU Hongrui WANG Ziqiang SONG Biao,a new Shrimp age of the Xia-maling Formation in the North China Plate and its geological signillcanee,Acta Geologica Sinica,2006(06).
[41]  GAO Linzhi;YIN Chongyu;WANG Ziqiang.New view of the Neoproterozoic strata on the southem margin of the North China Platform[J].Regional Geology of China,2002(03)
[42]  尹崇玉;王砚耕;唐烽;万渝生 王自强 高林志 邢裕盛 刘鹏举.贵州松桃南华系大塘坡组凝灰岩锆石SHRIMP ⅡU-Pb年龄[J].地质学报,2007(02)
[43]  尹崇玉.国际新元古代年代地层学研究进展与发展趋势[J].地层学杂志,2005(02)
[44]  邢裕盛;刘桂芝;乔秀夫;王自强, 全秋其,中国的上前寒武系,北京:地质出版社,1989.
[45]  邢裕盛;段承华;梁玉左;曹仁关,中国晚前寒武纪古生物,北京:地质出版社,1985.
[46]  邢裕盛;刘桂芝,中国晚前寒武纪微古植物群及其地质意义,中国地质科学院院报,1982(04).
[47]  邢裕盛;刘桂芝,燕辽地区震旦纪微古植物群及其地质意义,地质学报,1973(01).
[48]  邢裕盛,中国震旦系.《国际交流地质学术论文集(2),地层、古生物》,北京:地质出版社,1979.
[49]  宋彪;张玉海;万渝生,锆石SHRIMP样品靶制作、年龄测定及有关现象讨论,地质论评,2002(zk).
[50]  全国地层委员会,<晚前寒武纪地层分类命名会议>纪要,地层学杂志,1983(01).
[51]  乔秀夫;高林志;张传恒.中朝板块中、新元古界年代地层柱与构造环境新思考[J].地质通报,2007(05)
[52]  乔秀丈,青白口系地层学研究,地质科学,1976(04).
[53]  陆松年;杨春亮;李怀坤.华北占大陆与哥伦比亚超大陆[J].地学前缘,2002(04)
[54]  柳永清;高林志;刘燕学;宋彪 王宗秀.徐淮地区新元古代初期镁铁质岩浆的锆石U-Pb定年[J].科学通报,2002(22)
[55]  刘鸿允,中国震旦系,北京:科学出版社,1991.
[56]  刘敦一;简平;张旗;张福勤 石玉若 施光海 张履桥 陶华.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,2004(03)
[57]  李明荣;王松山;裘冀,京津地区铁岭组、景儿峪海绿石40Ar-39Ar年龄,岩石学报,1996(03).
[58]  耿元生;杨崇辉;杜利林;王新社 任留东 周喜文.天宝山组形成时代和形成环境-锆石SHRIMP U-Pb年龄和地球化学证据[J].地质论评,2002(04)
[59]  ZHANG Chuanheng;GAO Linzhi;WU Zhenjie;SHI Xiaoying YAN Quanren LI Dajian.SHRIMP U-Pb zircon age of tuff from the Kunyang Group in central Yunnan:Evidence for Grcnvillian orogeny in South China[J].Chinese Science Bulletin,2004(08)doi:10.1007/s11434-007-0225-x
[60]  高林志;张传恒;史晓颖;工自强, 刘耀明,华北古陆下马岭组归属中元古界的SHRIMP锆石新证据,科学通报,2008.
[61]  陈晋镳;张惠民;朱世兴;赵震, 王振刚,蓟县震旦亚界的研究,天津:天津科学技术出版社,1980.
[62]  DU Lilin;GENG Yuansheng;YANG Chonghui;WANG Xinshe,BEN Liudong,ZHOU Xiwen,SHI Yuruo,YANC Zhusheng.Geochemistry and SHRIMP U-Pb zircon hronology of basalts form the Yanbian Group in the western Yangtze Block[J].Acta Geologica Sinica,2005(06)
[63]  YIN C;TANG F;LIU Y;GAO L LIU P XING Y YANG Z WANG Z,U-Ph zircon age from the base of the Ediacaran Doushantuo Formation in the Yangtze Gorges,South China:constraint on the age of Marinoan glaciation,Episodes,2004(01).
[64]  LUDWIG K R,SQUID 1.02,a user\'s manual,Berkeley Geochronology Centre,Special Publication,2002.
[65]  Lu S N;Zhao G C;Wang H C,Precambrian metamorphic basement and sedimentary cover of the North China Craton,Precambrian Research? ,2008, 160.
[66]  高林志;乔秀夫,震旦系,北京:地质出版社,2005.
[67]  YIN Changyu;LIU Pengju;TANG Feng;GAO Linzhi.Advances in the Study on the Chronostratigraphy of the Ediacaran Peried in the World and Developments in Future[J].Geological Review,2006(06)
[68]  XING Yusheng;GAO Zhenjia;WANG Ziqiang;GAO Linzhi, YIN Changyu,The Neeproterosoic Erathem (Part 4),北京:地质出版社,2000.
[69]  XING Yusheng;DUAN Cbenghua;LIANG Yuzuo;CAO Rengnan,Late Precambrian Paloonology of China.People\' s Republic of China Ministry of Geology and Mineral Resources,geological Memoirs,series(2),number(2),北京:地质出版社,1985.
[70]  WANG Yuelun;LU Zonghin;XING Ynsheng;GAO Zhenjia, LIN Weixing, MA Guogan, ZHANG Luyi, LU Sangnian,Subdivision and correlation of the Upper Precambrian in China,天津:天津科学技术出版社,1980.
[71]  杜利林;耿元生;杨崇辉;王新社 任留东 周喜文 石玉若 杨铸生.杨了地台西缘盐边群玄武质岩石地球化学特征及SHRIMP锆石U-Pb年龄[J].地质学报,2006(06)
[72]  高维;张传恒;高林志;史晓颖 刘耀明 宋彪.北京密云环斑花岗岩锆石SHRIMP U-Pb年龄及其构造意义[J].地质通报,2007(06)
[73]  高林志;张传恒;史晓颖;周洪瑞 王自强.华北青白口系下马岭组凝灰岩锆石SHRIMP U-Pb定年[J].地质通报,2007(03)
[74]  SRACEY J S;KRAMERS JD,Approximation of terrestrial lead isotope evolution by two-stage model,earth planet,Science Letters,1975.
[75]  QIAO Xiufu ;GAO Linzhi ;PENG Yang,Mesoproterozoic Earthquake Events and Breakup of the Sino-Korean Plate,Acta Geologica Sinica?,2007, 81(3).
[76]  QIAO Xiufu;GAO Linzhi;PENG Yang,Neoprotemzoie in Paleo Tanlu fault zooe-Catastrophe,sequences,Biostratigraphy,北京:地质出版社,2001.
[77]  LU Songnian;LI Huaikun;CHEN Zhihong,Relationshi between Neorotemzoic crotons of China and the Rodinia,Earth Sciences Frontiers,2004(02).
[78]  LIU Dunyi;JIAN Ping;ZHANG Qi;ZHANG Fuqin SHI Yuruo SHI Gnanghai ZHANG Nuqiao TAO Hua.SHRIMP Dating of Adakites in the Tulingkai Ophiolite,Inner Mongolia:Evidence for the Early Paleozoic Subduction[J].Acta Geologica Sinica,2007(03)
[79]  LI Mingrong;WANG Lunshan;JI Qiu,The Ages of Glaueonites from Tiering and Jingeryu Formations,Beijing~Tianjin Area,Acta Petrologica Sinica,1996(03).
[80]  LIU Hongyun,The Sinian System in China,北京:科学出版社,1991.
[81]  LEE J S;CHAOYT,Geology of the Gorge District of the Yangtze(from Iehang to Tsekuei)with special referenceto development of the Gorges,Bulletin of the Geological Society of China,1924(3-4).
[82]  Black LP. ;Kamo SL. ;Williams IS. ;Mundil R. ;Davis DW. ;Korsch RJ. Foudoulis C.,The application of SHRIMP to Phanerozoic geochronology; a critical appraisal of four zircon standards,Chemical geology?,2003, 200(1-2).
[83]  KAO C S;HSIUGYH;KAOP,Preliminary notes on Sinian stratigraphy of North China,Bulletin of Geological Society of China,1934.
[84]  GENG Yuansheng;YANG Chonghui;WANG Xinshe;DU Lilin ZHOU Xiwen.Age of crystalline basement in Western Margin of Yangtze Terrane[J].Geological Journal of China Universities,2008(03)
[85]  GAO Linzhi;ZHANG Chuanheng;SHl Xiaoying;ZHOU Hongrui WANG Ziqiang.Zircon SHRIMP U-Pb dating of the ashbed from Xiamaling Formation,Qingbaikou Group in North China[J].Geological Bulletin of China,2007(03)
[86]  CLAOUE-LONG J C;COMPSTON W;ROBERTS J;FANNING C M,Two Carboniferous Ages:a Comparison of SHmMP Zircon Dating with Conventional Zircon Ages and 40Ar/39Ar Analysis,SEPM Special Publication,1995.
[87]  CHEN Jinbiao;ZHANG Huimin;ZHU Shixing;ZHAO Zhen,WANG Zhengang,Research on Sinian Suberathem of Jixian,Tianjin,天津:天津科学技术出版社,1980.
[88]  张传恒;武振杰;高林志;史晓颖 阎全人 李大建.滇中昆阳群凝灰岩锆石SHRIMP U-Pb年龄:华南格林维尔期造山的证据[J].科学通报,2006(07)
[89]  尹崇玉;柳水清;高林志;王自强, 唐烽, 刘鹏举,震旦(伊迪卡拉)纪早期磷酸盐化生动物群--瓮安生物群特征及其环境演化,北京:地质出版社,2007.
[90]  尹崇玉;刘鹏举;唐烽;高林志.国际埃迪卡拉系年代地层学研究进展与发展趋势[J].地质论评,2007(06)
[91]  邢裕盛;尹崇玉;高林志,震旦系的范畴、时限及内部划分,现代地质,1999(02).
[92]  邢裕盛;高振家;王自强;高林志, 尹崇玉,中国地层典,新元古界,北京:地震出版社,1996.
[93]  王日仑;陆宗斌;邢裕盛;高振家, 林蔚兴, 马国干, 张录易, 陆松年,中国卜前寒武系的划分和对比,天津:天津科学技术出版社,1980.
[94]  王鸿祯;张世红.全球前寒武系基地构造格局与古大陆再造问题[J].地球科学-中国地质大学学报,2002(05)
[95]  王鸿祯,关于国际(年代)地层表与中国地层区划,现代地质,1999(02).
[96]  邓晋福;莫宣学;赵海玲;罗照华, 吴宗絮,中国大陆根--柱构造:大陆动力学的钥匙,北京:地质出版社,1996.
[97]  乔秀夫;高林志;彭阳,古郯庐带新元古界--灾变、层序、生物,北京:地质出版社,2001.
[98]  陆松年;李惠民,蓟县长城系大红峪组火山岩的单颗粒锆石U-Pb法准确定年,中国地质科学院院报,1991.
[99]  陆松年;李怀坤;陈宏;于海峰 金巍 郭坤一.新元古时期中国古大陆拼合与罗迪尼亚超大陆的关系[J].地学前缘,2008(02)
[100]  李怀坤;李惠民;陆松年,长城系团山子组火山岩颗粒锫石U-Pb年龄及其地质意义,地球化学,1995(10).
[101]  耿元生;杨崇辉;王新社;杜利林 周喜文.杨子地台西缘结晶基底的时代[J].高校地质学报,2000(03)
[102]  YIN Chongyu;WANG Yangang;TANG Feng;WAN Yusheng WANG Ziqiang Gao Linzhi XING Ynsheng LIU Pengju,SHRIMP Ⅱ U-Pb Zircon Date from the Nanhuan Datangpo Formation in Songtao County,Guizhou Province,Acta Geologica Sinica,2002(02).
[103]  YIN Chongyu;LIU Yongqing;GAO Linzhi;WANG Ziqiang, TANG Feng, LIU Pengiu,Phosphatized biota in early Sinian (Ediacaran)-Wang\' an biota and its environment,北京:地质出版社,2007.

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