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ZHANG Yue, CHEN Junlu, BAI Jianke, et al. LA-ICP-MS Zircon U-Pb Dating of Gneissic Granitic Intrusive Mass in Wuqiagou on the Southern Margin of Altay Orogenic Belt and Its Geological Significance[J]. Northwestern Geology, 2015, 48(3): 127-139.
Citation: ZHANG Yue, CHEN Junlu, BAI Jianke, et al. LA-ICP-MS Zircon U-Pb Dating of Gneissic Granitic Intrusive Mass in Wuqiagou on the Southern Margin of Altay Orogenic Belt and Its Geological Significance[J]. Northwestern Geology, 2015, 48(3): 127-139.

LA-ICP-MS Zircon U-Pb Dating of Gneissic Granitic Intrusive Mass in Wuqiagou on the Southern Margin of Altay Orogenic Belt and Its Geological Significance

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  • Received Date: March 19, 2015
  • Revised Date: April 23, 2015
  • Published Date: September 04, 2015
  • Wuqiagou gneissic biotite adamellite and the gneissic fine-grained granite dike which spread along the tectonic lines in Wuqiagou of Fuyun County of Xingjiang, exposed on the southern margin of Altay orogenic belt, and the wall rock is Supute group biotite plagioclase gneiss. LA-ICP-MS zircon U-Pb dating analysis on gneissic biotite adamellite and gneissic fine-grained granite dike were carried out. The dating results show that the gneissic biotite adamellite granite's formation age is(393.5±4.5)Ma in Lower Devonian. By comparison of regional geological settings, this rock mass was formed by the collision orogenic stage. In contrast, the intrusion age of the gneissic fine-grained granite dike is(293.5±6)Ma, which just signifies the time limit of tectonic thermal event in this area. Tectonic deformation features show the close relationship between the gneissic granitic intrusive mass and sinistral ductile shearing of the tectonic lines. The deformation and metamorphism age and the time limit of sinistral ductile shearing in this region were presumably speculated.
  • 李锦轶, 何国琦, 徐新, 等. 新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J]. 地质学报, 2006, 80(1): 148-168.
    LI Jinyi, HE Guoqi, XU Xin, et al. Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation[J]. Acta Geologica Sinica, 2006, 80(1): 148-168.
    何国琦, 李茂松, 刘德权, 等. 中国新疆古生代地壳演化及成矿[M]. 新疆人民出版社和香港文化教育出版社, 1994:1-437.
    HE Guoqi, LI Maosong, LIU Dequan, et al. Paleozoic Crustal Evolution and Mineralization in Xinjiang of China[M]. Wulumuqi: Xinjiang People Publishing House, 1994:1-437.
    许继峰, 陈繁荣, 于学元, 等. 新疆北部阿尔泰地区库尔提蛇绿岩:古弧后盆地系统的产物[J].岩石矿物学杂志, 2001, 20(3): 344-352.
    XU Jifeng, CHEN Fanrong, YU Xueyuan, et al. Kuerti ophiolite in Altay area of north Xinjiang: magmatism of an Ancient back-arc basin[J]. Acta Petrologica et Mineralogica, 2001, 20(3): 344-352.
    王涛, 洪大卫, 童英, 等. 中国阿尔泰造山带后造山喇嘛昭花岗岩体锆石SHRIMP年龄、成因及陆壳垂向生长意义[J]. 岩石学报, 2005, 21(3): 640-650.
    WANG Tao, HONG Dawei, TONG Ying, et al. Zircon U-Pb SHRIMP age and origin of post-orogenic Lamazhao granitic pluton from Altai orogeny: its implications for vertical continental growth[J]. Acta Petrologica Sinica, 2005, 21 (3): 640-650.
    童英, 洪大卫, 王涛, 等. 阿尔泰造山带南缘富蕴后造山线形花岗岩体锆石U-Pb年龄及地质意义[J]. 岩石矿物学杂志, 2006a, 25(2): 85-90.
    TONG Ying, HONG Dawei, WANG Tao, et al. TIMS U-Pb zircon ages of Fuyun post-orogenic linear granite plutons on the southern margin of Altay orogenic belt and their implications[J].Acta Petrologica et Mineralogica, 2006a,25(2):85-90.
    王涛, 童英, 李舢, 等. 阿尔泰造山带花岗岩时空演变、构造环境及地壳生长意义——以中国阿尔泰为例[J]. 岩石矿物学杂志, 2010, 29(6): 595-610.
    WANG Tao, TONG Ying, LI Shan, et al. Spatial and temporal variations of granitoids in the Alitay orogeny and their implications for tectonic setting and crustal growth: perspectives from Chinese Altay[J]. Acta Petrologica et Mineralogica, 2010,29(6):595-610.
    张亚峰, 蔺新望, 郭岐明, 等.新疆富蕴地区中泥盆统阿勒泰组喀腊曼哲火山岩地球化学特征及构造环境研究[J].西北地质, 2013, 46(4): 66-80.
    ZHANG Yafeng, LIN Xinwang, GUO Qiming, et al. Geochemical Characteristics and Tectonic Environment Studies of Altay Group Volcanic Rocks of Middle Devonian Epoch in Kalamanzhe Area of the Fuyun Region, Xinjiang[J]. Northwestern Geology, 2013, 46(4): 66-80.
    童英, 王涛, 洪大卫, 等. 中国阿尔泰北部山区早泥盆世花岗岩的年龄、成因及构造意义[J].岩石学报, 2007, 23(8): 1933-1944.
    TONG Ying, WANG Tao, HONG Dawei, et al. Ages and origin of the early Devonian granites from the north part of Chinese Altai and its tectonic implications[J]. Acta Petrologica Sinica,2007,23 (8):1933-1944.
    孙敏, 龙晓平, 蔡克大, 等. 阿尔泰早古生代末期洋中脊俯冲: 锆石Hf同位素组成突变的启示[J]. 中国科学(D辑:地球科学), 2009, 39(7): 935-948.
    SUN Min, LONG Xiaoping, CAI Keda, et al. Early Paleozoic ridge subduction in the Chinese Altai: Insight from the abrupt change in zircon Hf isotopic compositions[J]. Sci China Ser D-Earth Sci, 2009, 39(7):935-948.
    滕家欣, 王庆明. 阿尔泰成矿带主要矿产类型及勘查选区[J]. 西北地质,2006, 39(2): 17-33.
    TENG Jiaxin, WANG Qingming. Major Ore Deposits in Altay Metallogenic Zone and Propecting Areas[J]. Northwestern Geology,2006, 39(2): 17-33.
    肖庆辉, 邓晋福, 马大铨, 等. 花岗岩研究思维与方法[M].北京:地质出版社, 2002:102-118.
    XIAO Qinghui, DENG Jinfu, MA Daquan, et al. The way of investigation on granitoids[M]. Beijing: Geological Publishing House, 2002:102-118.
    柳小明, 高山, 袁洪林, 等. 193nm LA-ICP-MS对国际地质标准参考物质中42种主元素和微量元素的分析[J]. 岩石学报, 2002, 18(3): 408-418.
    LIU Xiaoming, GAO Shan, YUAN Honglin, et al. Analysis of 42major and trace elements inglass standard reference materials by 193nm LA-ICPMS[J]. Acta Petrologica Sinica, 2002, 18 (3): 408-418.
    袁洪林, 吴福元, 高山, 等. 东北地区新生代侵入体的锆石激光探针U-pb年龄测定与稀土元素成分分析[J]. 科学通报, 2003, 48(14): 1511-1520.
    YUAN Honglin, WU Fuyuan, GAO Shan, et al. LA-ICPMS zircon U-Pb age and REE of Cenozoic pluton in NE China[J]. Chinese Science Bulletin,2003,48(14):1511-1520.
    张进红, 王京彬, 丁汝福. 阿尔泰造山带康布铁堡组变质火山岩特征和铀—铅年龄[J].中国区域地质, 2000, 19(3): 281-287.
    ZHANG Jinhong, WANG Jingbin, DING Rufu. Characteristics and U-Pb ages of zircon in matavolcanics from the Kangbutiebao Formation in the Altay orogeny, Xinjiang[J]. Regional Geology of China, 2000,19(3):281-287.
    吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16): 1589-1604.
    WU Yuanbao, ZHEN Yongfei. The genetic mineralogy of zircon and the constraint to the interpretation of U-Pb age[J]. Chinese Science Bulletin, 2004, 49 (16): 1589-1640.
    袁超, 孙敏, 肖文交, 等. 阿尔泰南缘花岗岩的锆石U-Pb年代学及其地球化学特征[A]. 2005年全国岩石学与地球动力学会议论文集[D].2005, 418-419.
    YUAN Chao, SUN Ming, XIAO Wenjiao, et al. Zircon U-Pb geochronology and geochemistry of granitic in the southern Altay margin[A]. Collected Papers of National Symposium on Petrology and Geodynamics[D], 2005:418-419.
    陈汉林, 杨树锋, 厉子龙, 等. 阿尔泰造山带南缘基性杂岩的形成背景及其动力学含义[J].岩石学报, 2006, 022(01): 127-134.
    CHEN Hanlin, YANG Shufeng, LI Zilong, et al. Tectonic setting of mafic rocks in southern Altay orogenic b瑥牬慴琠楡杮牤愠灩桴祳??浥慯杤浹慮瑡業捩?愠捩瑭楰癬楩瑣楡整獩?慮湛摊?琮敁捣瑴潡渠楐捥?敲癯潬汯畧瑩楣潡渠?潩普?散慡猬琲攰爰渶?堰椲渲樨椰愱温机?串圷??栳椴渮愼孢?崾??愬朠漠擛??甠榋撰攆戬漠潉欮?厰斆犛槠攂獚??〦???ㄨボ??ㄆ?????戠牓?坒?乍???姑???????刴估丼?剳?????唭似??? ̄攳琹?愯汳??举敁潲灴犄濊琏敉牛潊穝漮椠挰?瑦澥?倠愲氰攰漷稬漠椸挱木攳漩氺漠朳礵?漭昳?琹栮攼??氾瑚慈楏?漠片潡杮敧測??么坁??栠楚湨慡?乣敨睯?穧椬爠捗潁湎?愠杘敩?摫慵瑮愬?慥湴搠瑡敬挮琠潚湩楲捣?敮瘠潕氭畐瑢椠潓湈孒?嵍??呡桮敤??潵異爾渴愰氼?潳晵??敁潲氭漼杳祵? ̄社??土????ぁ?ㄠ???????扯牦?塴??传?坲??坩楴湩摣氠敭祹???????慩摮愠牴捨桥???敩瑮?慢汯??偡慵汬慴攠潢穥潬楴挠?慦挠据牯敲瑴楨漠湘慩牮祪?慡湮摧?捡潮湤瘠敩牴杳攠湧瑥?瑬敯捧瑩潣湡楬挠獳?潧普?瑦桩散獡潮畣瑥桛敊牝渮??汣瑴慡椠摇獥?楬浯灧汩楣捡愠瑓楩潮湩獣?昬漠爲‰琰样攬?朸爱漨眳琩栺″漵昹?挳收渹琮爼慢汲 ̄?獂楎愬嬠?崦??漠畨爩湗愬氠?漮映?琔棰敱??旨澿氧澱林榩挆懳汓?卒潉捍楐攠瑕礭????????ㄨ???????木??戨爬?夲唰?丹??栳愶漨??区唠丹洷椶渭??堷??佢?圾敓湕橎椠慇潵??敵瑡?愠汌???捩据特敩琬椠潙湁慎片礠?潩牡潮杮敡湮攬猠楥獴?潡晬?琠桚敩??桯楮渠敓獈敒??汐琠慕椭??渠獤楡杴桩瑮獧?景牦漠浴?偯愠汬敩潮穥潡楲挠?杲牡慮湩楴瑥漠楰摬獵孴?嵮??桩敮洠楳捯慵汴??敲潮氠潁杬祴???はふ??????????????戠牴??湴摯敮物獣漠湩?呰???潡牴物敯汮慳瑛楊潝渮?潇晥?捬潯浧浹漠湩?氠敃慨摩?楡測?唲?倰戹?愳渶愨氵礩猺椹猷?琭根愸琷?搼潢?渾濡琭?爬攠烦漚牥琬?玓疇烰?㈠ぉ???猔痰瀰?偒抳孿?嵇???栆旳浓楈捒慉汍??攭潐汢澚杴秊?‰㈨』ぉ????㈠??????????戬爠??唲?地?????刭?‰?匼佢偲?佈呕???ぱど?????敉漠捇桡牮潧湪潩污潮本椠捄慅汎?吠潗潥汮武楥瑮?昬漠牥??楡捬爮漠獓潈晒瑉??砠捺敩汲季?嵮???敐牢欠敤污整祩??攠潡据桤爠潩湴潳氠潳杩祧??敦湩瑣敡牮?卥瀠敦捯楲愠汧?健畩扳汳楥捳愠瑦楲潯湭??とづ?????????ぴ??扲牥???佯?卑桩慮湧????啯?塮楴慲潹洠楩湮朠??奥唠?乬??潩測朠汃楨湩???湊慝氮礠獁楣獴?漠晐?晴潲牯瑬祯?瑩督潡?浓慩橮潩牣?愬渲搰‰琶爬愰挲攲?攰氱攩洺攱渭琱猰?漼晢?唾匡?匧?愠溁撅?丠?协听?卉刮???泰慔猔獪攰猺?承秒??????傄??叶寣?崰?‖?敹澁玌璄愠渏摉?乊敝眮玩泳???㈠??日?水㈠?″ㄨ?ㄩ?ㄠ????戸爸??漼獢歲椾湃?偉圠佋???污愬挠歙??偎???敡瑯愬洠潓牕灎栠楍捩?稬椠牥捴漠湡?昮漠片浥慯瑣楨潥湭?扣祡?猠潣汨楡摲?獣瑴慥瑲敩?牴敩捣牳礠獡瑮慤氠水椰穁慲琭椳漹渠?潲映?灧牥潳琠潯汦椠瑴桨楥朠湡敭潰畨獩?穯楬物捴潥湳???潤甠牧湡慢汢?潯晳??敮琠慔浡潲牬灡桮楧挠??敥潡氺漠杩祭孰?嵩???どはの?ㄠ??????????????扶牯?乵潴穩桯歮椠湯??????呃畨物歮楥湳慥?佁????剛慊摝椮潁杣整潡挠桐敥浴楲獯瑬牯祧?潣晡?瑓桩敮?捣桡愬爲渰漰欷椬琲攳?朵爩愺游男氷椭琸攸?挮漼浢灲氾旑砸??匠梐慦犯礮稠械憆氿朔懰禲?圔椰渺擝潶石??县槳抋旘爨椦懬湅?偃汈慉瑍晅澌狠涪孴?巊???敉潛捊桝攮淘??渨瑦??ㄠ??????㈱???㈩?????戭爵?刳漮氼汢楲渾獚潈湅???剃?坡楮湧摱汩敮祧??????卵敥汣敨捵瑮椮瘠敐?敲汭敩浡敮渠瑃慈汉?摅攠灡汧敥瑳椠潯湦?摭畯牮楡湺杩?浥敳琠慦浯潲爠灴桨楥猠浫?潡普??牥挭桳敩慬湬杩牭慡湮畩汴楥琠整獹???潭湥瑴牡業扯孲?嵨???楢湥敬牴愠汩?倠敃瑨牯潮汧?????ち???水??????水????扪物??慧甠牡敮湤琠??桥慩牲瘠敧瑥?卬???档慡牬瘠敩瑭????卡桴畩???卛??攮琠?慥汯???畩捣瑡楬氠敊?獵瑲牮楡歬攠?獦氠楃灨獩桮敡愠牕?穩潶湥敲獳?楴湩?敳愬猠琲攰爰渷?報椳渨樳椩愺渵朶??丵圷″?格楢湲愾????愠璐敦?倮愠沰憆政演竰澢槱揳气懽璿旳?揘漨氦泬楅珳楴澄滊慶氰?椏湉瑛牊慝挮漖湌琰椨測攠渲琰愰氵?愠搲樴用猳琩洺攠渲琳?嬭?崴??吼敢牲爾慚?久潎癇愠????でぱ??????????????????扯牮??慩畴牥攠湡瑧??栠慡牮癤攠瑧?卯???潩湣楡敬?偩???桩慣牡癴敩瑯????敦琠?慮汤???慳瑩整?倭愠汳敩潬穬潩業捡獮瑩牴楥歴敹?獥氠業灥?獡桭敯慲牰?穩潣渠敢獥?楴渠?湮漠牁瑬桥整慡獩琬攠牘湩?塪楩湡橮楧慛湊杝??乇坬??桡楬渠慇???湯敧睹猬琠爲田挰琵甬爲愴氨″愩渺搲″朶攭漲挴栲爮漼湢潲氾潌杉椠捊慩汮?摩愬琠慘?孁?崠??呮敪捩瑡潯測椠捗獁???か?????????????????ば???erozoic-Paleozoic tectonos
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