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地质学报  2009 

华北陆块东北缘张三沟岩组SHRIMP锆石U-Pb年代学研究及其地质意义

, PP. 642-650

Keywords: SHRIMP年代学,张三沟岩组,华北陆块东北缘,吉林

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Abstract:

出露于华北陆块东北缘的张三沟岩组为一套变质火山-沉积岩系,前人根据变质程度和地层对比将其划归古元古代。本文通过SHRIMP锆石U-Pb年代学研究,获得2517±9Ma、2518±7Ma和2534±26Ma原岩年龄,2439±24Ma、2464±73Ma和2433±71Ma变质年龄。这表明该套变质岩层形成于新太古代晚期,变质时代在新太古代末-古元古代初。结合区域资料,其变质年龄可能代表了古龙岗陆块与位于其北东侧的其它陆块(如佳木斯陆块)碰撞造山的时代,表明华北克拉通在新太古代末-古元古代初期经历过一次重要的克拉通化。

References

[1]  白瑾 黄学光 等.中国前寒武纪地壳演化(第一版)[M].北京:地质出版社,1993.230.
[2]  陈道公 倪涛.大别-苏鲁造山带高级变质岩中锆石微区U,Th和Pb化学组成特征统计[J].岩石学报,2004,20(5):999-1006.
[3]  陈跃军 花艳秋 李林山 黄贤玉 刘跃文 李睿.吉林敦化小蒲柴河地区张三沟岩组的建立[J].世界地质,2005,24(2):144-148.
[4]  沈保丰 李俊建 等.吉林夹皮沟金矿地质与成矿预测[M].北京:地质出版社,1998.108-116.
[5]  翟明国 卞爱国.华北克拉通新太古代末超大陆拼合及古元古代末―中元古代裂解[J].中国科学:D辑,:.
[6]  赵国春.华北克拉通基底构造单元特征及早元古代拼合[J].中国科学:D辑,:.
[7]  周晓东 殷长建.吉林省近期基础地质研究新进展[J].吉林地质,2004,23(4):1-18.
[8]  Li J H, Kusky T. 2007. A Late Archean foreland fold and thrust belt in the North China Craton: Implications for early collisional tectonics. Gondwana Research, 12: 47-66.
[9]  Li S Z, Zhao G C, Sun M, Wu F Y, Hao D F, Han Z Z, Luo Y, Xia X P. 2005. Deformational history of the Paleoproterozoic Liaohe Group in the Eastern Block of the North China Craton. In. Wilde, S A, Zhao G C (Eds.), Late Archean to Paleoproterozoic Evolution of the North China Craton. J. Asian Earth Sci. , 24, 659-674.
[10]  Ludiwg K R. 2002. Squid 1. 02: A user manual. Berkeley Geochronological Center Special Publication, No. 2: CA94709, USA.
[11]  Ludiwg K R. 1999. Using Isoplot/EX version 2:a geochronologicai toolkit for Microsoft Excel. Berkeley Geochronological Center Special Publication, 1a: 47.
[12]  LuoY, SunM, ZhaoG C, LiSZ, Xu P, Ye K, Xia XP. 2004. LAICP-MS U-Pb zircon ages of the Liaohe Group in the Eastern Block of the North China Craton: constraints on the evolution of the Jiao-Liao-Ji Belt. Precambrian Res. 134, 349-371.
[13]  MiaoLC, Qiu Y M, Fan W M, Zhang F Q, Zhai M G. 2005. Geology, geochronology, and tectonic setting of the Jiapigou gold deposits, southern Jilin Province, China. Ore Geology Reviews, 26 : 137-165.
[14]  Mojzsis S J, Harrison T M. 2002. Establishment of a 3. 83 Ga magmatic age for the Akilia tonalite ( southern West Greenland). Earth and Planetary Science Letters, 202:563- 576.
[15]  Song B, Nutman A P, Liu D Y, Wu J S. 1996. 3800 to 2500 Ma crustal evolution in the Anshan area of Liaoning Province, northeastern China. Precambrian Research, 78: 79-94.
[16]  Tatsumi Y and Ishizaka K andesites in the Setouchi 1982. Origin of high-magnesian volcanic belt, southwest Japan: I. Petrographical and chemical characteristics. Earth Planet Sci Lett, 60: 293-304.
[17]  Vavra G, Gebarer Dand Schmid R, Compston W. 1996. Mul zircon growth and recrystallization during polyphase Carboniferous to Triassic metamaorphism in granulites of Ivrea Zone (Southern Alps) : an study. Contrib. Mineral. Petrol., tipl Lat th ion microprobe (SHRIMP) 122: 337-358.
[18]  Vavra G, Schmid R, Gebauer D. 1999. Internal morphology, habit and U-Th-Pb microanalysis of amphibole to granulite facies zircon: Geochronology of the Ivren Zone (Southern Alps). Contrib Mineral Petrol, 134: 380-404.
[19]  戴新义 刘劲鸿 邵建波 蒋荣青.吉林夹皮沟-金城洞花岗岩-绿岩带的地质特征[J].前寒武纪地质,1990,9(4):51-60.
[20]  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.
[21]  李承东 张福勤 苗来成 等.吉林色洛河群的重新认识[J].吉林大学学报:地球科学版,2007,37(5):841-847.
[22]  李承东.[D].图书馆,中科院地质与地球物理研究所,2005.1-119.
[23]  李江海 侯贵廷 等.华北克拉通对前寒武纪超大陆旋回的基本制约[J].岩石学报,:.
[24]  李江海 钱祥麟.华北陆块基底构造格局及早期大陆克拉通化过程[J].岩石学报,:.
[25]  李俊建 沈宝丰 李双保 毛德宝.清原-夹皮沟绿岩带地质及金的成矿作用[M].天津:天津科学技术出版社,1994.1-132.
[26]  李三忠 刘永江 白立新 等.辽东古元古代变质基性侵入岩特征及其大地构造意义[J].西北大学学报,1997,27(增刊):442-445.
[27]  李三忠 刘永江 等.辽吉地区古元古代造山作用的大陆动力学过程及其壳内响应[J].地球物理学报,1998,41(增刊):142-152.
[28]  孙晓明 徐克勤 任启江 ReidR Keays.吉南太古界高级变质地体及金矿床[M].北京:地质出版社,1996.1-47.
[29]  吴昌华 钟长汀.华北陆台中段吕梁期的SW―NE向碰撞[J].前寒武纪研究进展,:.
[30]  伍家善 耿元生 沈其韩 万渝生 刘敦一 宋彪.中朝古大陆太古宙地质特征及构造演化(第一版)[M].北京:地质出版社,1998.1-212.
[31]  Rowley D B, Xue F, Tucker R D. 1997. Ages of ultrahigh pressure metamorphism and protolith orthogneisses from the eastern Dabie Shan= U/Ph zircon geochronology. Earth and Planet Science Letters, 151: 191-203.
[32]  Vavra G. 1994. Systematics of internal zircon morphology in major variscan granitoid types. On tribution to Mineralogy and Petrology, 117: 331-344.
[33]  Williams I S. 1998. U-Th Pb geochronology by ion microprobe. In: Mckibben Ma et al. (eds). Application of Microanalytical Technique to Understanding Mineralizing Process. Reviews in Economic Geology, 7: 1-35.
[34]  Wu Y B, Zheng Y F. 2004. Genesis of zircon and its constraints on interpretation of U-Ph age. Chinese Science Bulletin, 49 (15) 1554-1569.
[35]  Yogodzinski G M, Kay R W, Volynets O N, Koloskov A V, Kay S M. 1995. Magnesian andesite in the western Aleutian Komandorsky region: Implications for slab melting and processes in the mantle wedge. Geol. Soc. Am. Bull. , 107: 505-519.
[36]  Zhai M G, Liu W J. 2003. Paleoproterozoic tectonic history of the North China craton: a review. Precambrian Research, 122:183 -199.
[37]  Zhai M G, Guo J H, Liu W J. 2005. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton: a review. Journal of Asian Earth Sciences, 24 : 547-561.
[38]  Zhang Y B, Wu F Y, Simon A W, Zhai M G, Lu X P, Sun D Y. 2004. Zircon U - Pb ages and tectonic implications of \\'Early Paleozoic\\' granitoids at Yanbian, Jilin Province, northeast China[J]. The Island Arc 13, 484-505.
[39]  Zhao G C , Wilde S A , Cawood P A , Cawood P A , Sun M. 2001. Archean blocks and their boundaries in the North China Craton lithological , geochemical , structural and P -T path constraints and tectonic evolution. Precambrian Res. , 107: 45-73.

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