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地质学报  2007 

阿尔金北缘枕状玄武岩的地质特征及其锆石U-Pb年龄

, PP. 787-794

Keywords: 阿尔金,枕状玄武岩,蛇绿岩,地质特征,锆石U-Pb年龄

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Abstract:

阿尔金山北缘恰什坎萨依出露的玄武岩具枕状、气孔和杏仁状构造,镜下多为间隐结构,岩石化学成分特点及REE等微迹元素显示洋岛玄武岩特征;其颗粒锆石U-Pb年龄为448.6±3.3Ma。该区玄武岩与相伴产出的蛇纹石化橄榄岩、辉长岩及硅质岩、粉砂岩等呈断层接触关系,它们共同组成了较标准的蛇绿岩。这为探讨阿尔金山的大地构造演化提供了新的证据。

References

[1]  陈宣华,Gehrels G,王小凤,杨风,陈正乐.2003.阿尔金山北缘花岗岩的形成时代及其构造环境探讨.矿物岩石地球化学通报,22(4):294~298.
[2]  程裕淇.1994.中国区域地质概论.北京:地质出版社,517.
[3]  崔军文,唐哲民,邓晋福,岳永君,孟令顺,余钦范,李冀湘,赖绍聪,齐立,郭耕成,卢德源,朱红.1999.阿尔金断裂系.北京:地质出版社,137~249.
[4]  刘永江,葛肖虹,Genser J,Neubauer F,Friedl G,常丽华,Handler R.2003.阿尔金断裂带构造活动的40Ar/39Ar年龄证据.科学通报,48(12):1335~1341.
[5]  陆松年,李惠民.1991.蓟县长城系大红峪组火山岩的的单颗粒锆石U-Pb法准确定年.中国地质科学院院报,第22号,137~146.
[6]  陆松年主编.2002.青藏高原北部前寒武纪地质初探.北京:地质出版社,1~125.
[7]  张旗,周国庆.2001.中国蛇绿岩.北京:科学出版社,182页.
[8]  杨经绥,吴才来,史仁灯.2002.阿尔金山米兰红柳沟的席状岩墙群:海底扩张的重要证据.地质通报,21(2):69~74.
[9]  刘良,车自成,王焰等.1996.阿尔金山西段榴辉岩的确定及其地质意义.科学通报,41(14):1485~1488.
[10]  郑剑东.1991.阿尔金大地构造及其演化.现代地质,5(4):347-354.
[11]  Cheng Yuqi.1994.Conspectus of Chinese Regional Geology.Beijing:Geological Publishing House,517(in Chinese).
[12]  Guo Zhaojie,Zhang Z C,Wang J Q.1998.Sm-Nd isochron age of the ophiolite belt at the margin of the Altyn Tagh mountains and its tectonic signification.Chinese Science Bulletin,43(18):1981~1984(in Chinese with English abstract).
[13]  Hoffman A W,White W M.1982.Mantle plumes from anceient oceanic crust.Earth Planet.Sci.Lett.,57.421~436.
[14]  Liu Liang,Che Z C,Luo J H,et al.1996.Recogition and implication of eclogite in the western Altun mountain,Xinjiang.Chinese Science Bulletin,41(14):1485~1488(in Chinese with English abstract).
[15]  Liu Liang,Che Z C,Wang Y,et al.1999.The petrological characters and geotectonic setting of high-pressure metamorphic rock belts in Altun mountains.Acta Petrologica Sinica,15(1):57~64(in Chinese with English abstract).
[16]  Liu Liang.1999.High pressure metamorphic rocks and ophiolite in Altun,and its tectonic significance.The dissertation of PhD degree,Institute of Geology and Geophysics,CAS.1~70(in Chinese with English abstract).
[17]  Liu Yongjiang,Guo X H,Genser J,et al.2003.40Ar/39Ar age of tectonic activation of Altun fault.Chinese Science Bulletin,48(12):1335~1341(in Chinese with English abstract).
[18]  Lu Songnian,Li Huimin.1991.A precise U-Pb single zircon age determination for the volcanics of Dahongyu Formation,Changcheng System in Jixian.Bulletin of the Chinese Academy of Geological Sciences,22:137~146(in Chinese with English abstract).
[19]  Lu Songnian.2002.Preliminary study of Precambrian geology in the North Tibet-Qinghai Plateau.Beijing:Geological Publishing House,1~125(in Chinese with English abstract).
[20]  Pupin J P,et al.1980.Zircon and granite petrology.Contributions to Mineralogy and Petrology,73(3):207~220.
[21]  Ren Jishun,Xiao Liwei.2004.Lifting the mysterious veil of the tectonics of the Qinghai-Tibet Plateau by 1:250000 geological mapping.Geological Bulletin of China,23(1):1~11(in Chinese with English abstract).
[22]  Xiu Qunye,Yin Yanjie,Li Huimin.2000.Sampling and mineral sorting for single zircon U-Pb dating.Progress in Precambrian Research,23(2):168~175(in Chinese with English abstract).
[23]  Xu Zhiqin,Yang J S,Zhang J X,et al.1999.A comparison between the tectonic unites on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing.Acta Geologica Sinica,73(3):193~205(in Chinese with English abstract).
[24]  Yang Jingsui,Wu C L,Shi R D.2002.Sheeted dike swarm in Hongliugou,northwest of the Altun region:Evidence for seafloor spreading.Geological Bulletin of China,21(2):69~74(in Chinese with English abstract).
[25]  Yaoling Niu.2002.The origin of subduction zones:A new perspctive and implications for the global tectonics.In symposium on igneous rocks tectonics and mineralization at Tianjin institute of geology and mineral resources.
[26]  Yu Haifeng,Lu S N,Zhao F Q,et al.1998.Litho-structural evidences of ancient Altyn Tagh and its significance.Progress in Precambrian Research,21(4):10~14(in Chinese with English abstract).
[27]  Yu Haifeng,Lu S N,Liu Y S,et al.2002.Composing of the Altyn Tagh formation-complex and its tectonic signification.Geological Bulletin of China,21(12):834~840(in Chinese with English abstract).
[28]  Bevins R E,Kokelaar B P,Dunkley P N.1984.Petrology and geochemistry of lower to middle Ordovician igneous rocks in Wales:a volcanic arc to marginal basin transition.Proc.Geol.Ass.,95:337~347.
[29]  Bloomer S H,B Taylor,C J MacLeod,R J Stern,P Fryer,J W Hawkins,L Johnson.1995.Early arc volcanism and the ophiolite problem:A perspective from drilling in the western Pacific,in active margins and marginal basins of the western Pacific,edited.by Taylor B,and J H Natland,Geophys.Monogr.,88,1~30.
[30]  Bureau of Geology and Mineral Resources of Xinjinang Uygurl Autonomous Region.1993.Regional geology of Xinjinang Uygurl Autonomous Region.Beijing:Geological Publishing House,841(in Chinese with English abstract).
[31]  Che Zicheng,Liu L,Liu H F.1995.Discovery and occurrence of high-pressure metapelitic rock in Altun mountain area,Xinjiang Autonomous Region.Chinese Science Bulletin,40(14):1298~1300(in Chinese with English abstract)
[32]  Cui Junwen,Tan Z M,Deng J F,et al.1999.Altun Fault System.Beijing:Geological Publishing House,137~249(in Chinese with English abstract).
[33]  Dilek Y,Robinson P T.2003.Ophiolites in earth history.London:published by the Geological Society special publication,No.218,1~18.
[34]  Edward R Sobel,Nicolas Arnaud.1999.Apossible middle Paleozoic suture in the Altyn Tagh,NW China.Tectonics,18(1):64~74.
[35]  Ge Xiaohong,Zhang M S,Liu Y J,et al.1998.Scientific problems and thought for research of the Altun fault.Geoscience,12(3):295~301(in Chinese with English abstract).
[36]  Liu Liang,Sun Y,Xiao P X,et al.2002.Discovery of Ultrahigh pressure garnet pyroxene peridotite in Altyn Tagh.Chinese Science Bulletin,47(9):657~662(in Chinese).
[37]  Ren Jishun.2004.Some problems on the Kunlun-Qinling orogenic system.North Western Geology,37(1):1~5(in Chinese with English abstract).
[38]  Ren Shoumai,Guo X H,Liu Y J.2003.Progress in Altyn fault belts research.Advance in Earth Sciences,18(3):386~391(in Chinese with English abstract).
[39]  Rubatto D,Gebauer D.2000.Use of cathodoluminescence for U-Pb zircon dating by ION Microprobe:Some examples from the western Alps.Cathodoluminescence in Geoscience,Springer-Verlag,Berlin,Heidelberg,Germany.373~400.
[40]  Wang Xiang.1998.Quantitative description of zircon shape and its dynamic analysis.Science in China Series D,28(3):232~238(in Chinese with English abstract).
[41]  Wang Yunshan,Chen J N.1987.Metamorphic zone and metamorphism in Qinghai and adjacent area.Geological Special Bulletin(6),Ministry of Geology and Mineral resources,P R China.Beijing:Geological Publishing House,4~227(in Chinese with English abstract).
[42]  Wu Yuanbao,Zheng Y F.2004.Study on the genetic mineralogy of zircon and its constraint on the explanation on zircon U-Pb age.Chinese Science Bulletin,49(16):1589~1604(in Chinese with English abstract).
[43]  Xiao Xuchang,Tang Y Q,Feng Y M,et al.1992.Tectonics in northern Xijing and adjacent area.Beijing:Geological Publishing House,12~124(in Chinese with English abstract).
[44]  Zheng Jiandong.1991.Tectonics and evolution of Altyn Tagh orogeny.Geoscience,5(4):347~354(in Chinese with English abstract).
[45]  Yu Haifeng,Liu Y S,Xiu Q Y et al.2007.Frame of Precambrian key geological events in Altun mountains.Geological Bulletin of China(in press).
[46]  Zhang Jianxin.1998.Study on Caledonian orogenic root in western Altun orogeny.The dissertation of PhD degree,Chinese Acdemyog Geological Sciences(in Chinese with English abstract).
[47]  Zhang Qi,Xiao X C.1995.A comment on study of ophiolites in China.Acta Petrologica Sinica,11(Supp.):1~9(in Chinese with English abstract).
[48]  Zhang Q,Wang Y,Zhou G Q,Qian Q,paul T R.2003.Ophiolite in China:their distribution,ages and tectonic settings.In:Dilek Y,Robinson P T eds Ophiolite in earth history.London:published by the Geological society.Special publication,No.218,541~566.
[49]  Zhou Guoqing.1996.The concept of ophiolite and evolvement.In:Zhang Q,Ed.Ophiolite and Earth dynamics.Beijing:Geological Publishing House,15~20(in Chinese).
[50]  车自成,刘良,刘洪福,罗金海.1995.阿尔金山地区高压变泥质岩石的发现及其产出环境.科学通报,40(14):1298~1300.
[51]  车自成,刘良,罗金海编著.2002.中国及其邻区区域大地构造学.北京:科学出版社,207~369.
[52]  葛肖虹,张梅生,刘永江,等.1998.阿尔金断裂研究的科学问题与研究思路.现代地质,12(3):295~301.
[53]  郭召杰,张志诚,王建群.1998.阿尔金北缘蛇绿岩带的Sm-Nd等时线年龄及其地质意义.科学通报,43:1981~1984.
[54]  何国琦,李茂松,刘德权,等.1994.中国新疆古生代地壳演化及成矿.乌鲁木齐:新疆人民出版社,437.
[55]  赖绍聪,邓晋福,赵海玲.2000.青藏高原北缘火山作用与构造演化.西安:陕西科学技术出版社,74~96.
[56]  刘良,车自成,王焰,罗金海,陈丹玲.1999.阿尔金高压变质岩带的特征及其构造意义.岩石学报,15(1):57~64.
[57]  刘良.1999.阿尔金高压变质岩与蛇绿岩及其大地构造意义.中国科学院地质与地球物理研究所博士论文,1~70.
[58]  刘良,孙勇,肖培喜,车自成,罗金海,陈丹玲,王焰,张安达,陈亮,王永和.2002.阿尔金发现超高压(>3.8Gpa)石榴二辉橄榄岩.科学通报,47(9):657~662.
[59]  任纪舜,姜春发,张正坤,秦德余.1980.中国大地构造及其演化.北京:科学出版社,24~124.
[60]  任纪舜.2004.昆仑-秦岭造山系的几个问题.西北地质,37(1):1~5.
[61]  任纪舜,肖黎薇.2004.1:25万地质填图进一步揭开了青藏高原大地构造的神秘面纱.地质通报,23(1):1~11.
[62]  任收麦,葛肖虹,刘永江.2003.阿尔金断裂带研究.地球科学进展,18(3):386~391.
[63]  汪湘.1998.锆石形态的定量描述及其动力学分析.中国科学(D辑),28(3):232~238.
[64]  王云山,陈基娘.1987.青海省及毗邻地区变质带与变质作用.中华人民共和国地质矿产部地质专报第6号.北京:地质出版社,4~227.
[65]  吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589~1604.
[66]  肖序常,汤耀庆,冯益民,朱宝清,李锦轶,赵民.1992.新疆北部及其邻区大地构造.地质出版社,12~124.
[67]  新疆维吾尔自治区地质矿产局,1993,新疆维吾尔自治区区域地质志,北京:地质出版社,841.
[68]  修群业,殷艳杰.2000.单颗粒锆石年龄样品的采集及矿物分选.前寒武纪研究进展,23(2):168~175.
[69]  许志琴,杨经绥,张建新,姜枚,李海兵,崔军文.1999.阿尔金断裂两侧构造单元的对比及岩石圈剪机制.地质学报,73(3):193-205.
[70]  于海峰,陆松年,赵风清,李怀坤,郑健康.1998.古阿尔金断裂的岩石构造依据及意义.前寒武纪研究进展,21(4):10~14.
[71]  于海峰,陆松年,刘永顺,修群业,李铨.2002.阿尔金岩群组成及其构造意义.地质通报,21(12):834~840.
[72]  于海峰,刘永顺,修群业,李铨.2007.阿尔金山地区前寒武纪重大地质事件框架.地质通报(待刊).
[73]  周国庆.1996.蛇绿岩的概念及其演变.见:张旗主编.蛇绿岩与地球动力学研究.北京:地质出版社,15~20.
[74]  张建新.1998.阿尔金构造带西段加里东期山根的初步研究.中国地质科学院博士论文.
[75]  张旗,肖序常.1995.中国蛇绿岩研究概述.岩石学报,11(增刊):1~9.
[76]  左国朝,吴汉泉.1997.北祁连中段早古生代双向俯冲-碰撞造山模式剖析.地球科学进展,12:366~393.

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