东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义

吴昌志,张遵忠,Khin Zaw,Fernando Della-Pasque,唐俊华,郑远川,汪传胜,三金柱. 东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义[J]. 岩石学报, 2006, 22(5): 1121-1134.
引用本文: 吴昌志,张遵忠,Khin Zaw,Fernando Della-Pasque,唐俊华,郑远川,汪传胜,三金柱. 东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义[J]. 岩石学报, 2006, 22(5): 1121-1134.
WU ChangZhi~. Geochronology, geochemistry and tectonic significances of the Hongyuntan granitoids in the Qoltag area, Eastern Tianshan.[J]. Acta Petrologica Sinica, 2006, 22(5): 1121-1134.
Citation: WU ChangZhi~. Geochronology, geochemistry and tectonic significances of the Hongyuntan granitoids in the Qoltag area, Eastern Tianshan.[J]. Acta Petrologica Sinica, 2006, 22(5): 1121-1134.

东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义

  • 基金项目:

    本文受国家重点基础研究发展规划项目(2001CB409802)和国家自然科学基金(40472042)联合资助.

Geochronology, geochemistry and tectonic significances of the Hongyuntan granitoids in the Qoltag area, Eastern Tianshan.

  • 东天山觉罗塔格地区广泛发育的晚古生代岩浆岩及相关的矿产一直是东天山大地构造研究的焦点。觉罗塔格南缘红云滩花岗质岩体的岩石、矿物组合显示典型的钙碱性火山弧花岗岩特征。岩石地球化学研究表明,该花岗质岩石富集大离子亲石元素而亏损高场强元素,是洋壳俯冲所导致的下地壳物质部分熔融、岩浆分离结晶和上地壳同化混染作用的产物。LAM-ICP/MS锆石定年结果表明,红云滩花岗岩侵位于早-中石炭世(328.5±9.3Ma)。结合觉罗塔格地区由南至北,晚古生代矿产分布由火山沉积-热液改造型铁矿向斑岩型铜钼矿过渡的特征、火山-沉积岩分布和该区晚古生代的大地构造演化历史,作者推测:早古生代觉罗塔格洋向塔里木板块俯冲并形成中天山岛弧之后,该洋盆并未完全消亡,并于晚古生代时极性反转,向北俯冲于准-吐-哈地块之下。红云滩花岗岩正是形成于晚古生代觉罗塔格俯冲洋壳之上的火山弧环境。觉罗塔格地区晚古生代的岩浆岩,火山-沉积岩和矿产分布均不同程度受控于这一大地构造背景。
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  • [1]

    Bagby WC,Cameron KL,Cameron M.1981. Contrasting evolution of calc-alkalic volcanic and plutonic rocks of western Chihuahua,Mexico.J.Geophys.Res.,86:10402-10410

    [2]

    Barbarin B.1999. A review of the relationships between granitoid types,their origins and their geodynamic environments.Lithos,46:605 -626

    [3]

    Black LP and Gulson BL.1978. The age of the Mud tank Carbonatite,Strangways Range,Northern Territory.BMR Journal of Australian Geology and Geophysics 3:227-232

    [4]

    Black LP,Kamo SL,Allen CM,Davis DW,Aleninikoff JN,Valley JW,Mundil R,Campbell IH,Korsch RJ,Williams IS,Foudoulis C.2004. Improved 206pb/238 U microprobe geochronology by the monitoring of a trace-element related matrix effect; SHRIMP,IDTIMS,ELA-ICP-MS,and oxygen isotope documentation for a series of zircon standards.Chemical Geology,205,115-140

    [5]

    Black LP,Kamos L,Allen CM,Aleinikoff JN,Davis DW,Korsch RJ,Foudoulis C.2003. TEMORA 1:a new zircon standard for Phanerozoic U Pb geochronology.Chemical Geology,200:155 -170

    [6]

    Boynton WV.1984. Geochemistry of the rare earth elements:meteorite studies.In:Henderson P.(ed.),Rare earth element geochemistry.Elservier,66-114

    [7]

    Chappell BW,White AJR.1992. I-and S-type granites in the Lachlan Fold Belt.Trans.R.Soc.Edinb.Earth Sci.,83:1-26

    [8]

    Chen FW,He GQ,Li HQ.2003. Tectonic attribute of the Qoltag orogenic belt in the East Tianshan Mountains,northwestern China.Geology in China,30(4):361 -366 (in Chinese with English abstract)

    [9]

    Coleman R.1989. Continental growth of Northwest China.Tectonics,8:621-635

    [10]

    Ding TF.1990. The geological characteristics of stratabound iron deposits in the Yamasu formation in Xinjiang.Regional Geology of China,(3):369 -372 (in Chinese with English abstract)

    [11]

    Feng YM,Zhu BQ,Yang JL,Zhang KC.2002. Tectonic and evolution of the eastern Tianshan Mountains-a brief introduction to "tectonic map of the eastern Tianshan Mouintains of Xinjiang ".Xinjiang Geology,20(4):309 -314 (in Chinese with English abstract)

    [12]

    Ferrari L,Petrone CM,Francalanci L.2001. Generation of oceanicisland basalt type volcanism in the western Trans-Mexican volcanic belt by slab rollback,asthenosphere infiltration,and variable flux melting.Geology,29(6):507 -510

    [13]

    Gao J,Li MS,Xiao XC,Tang,YQ,He GQ.1998. Paleozoic tectonic evolution of the Tianshan orogen,northwestern China.Tectonophysics,287:213-231

    [14]

    Gao JF,Lu JJ,Lai MY Lin YP,Pu Wei.2003. Analysis of trace elements in rock samples uing HR-ICIMS,Journal of Nanjing University (Natural sciences),39(6):844 -850 (in Chinese with English abstract)

    [15]

    Gu LX Zhu JL,Guo JC,Liao JJ,Yan ZF,Yan H,and Wang JZ.1994. The east xinjiang-type mafic-ultramafic complexes in orogenic environments.Acta Petrologica Sinica,10 (4):339-356 (in Chinese with English abstract)

    [16]

    Gu LX,Hu Shouxi,Chu Qiang,Yu Chunshui and Xiao Xinjian.1999. Pre-collision granites and post-collision intrusive assemblage of the Kelameili-Harlik orogenic belt.Acta Geologica Sinica (English edition),73(3):316-329

    [17]

    Gu LX,Hu SX,Yu CS et al.2000. Carboniferous volcanites in the Bogda orogenic belt of eastern Tianshan:Their tectonic implications.Acta Petrologica Sinica,16 (3):305-316 (in Chinese with English abstract)

    [18]

    Gu LX,Hu SX,Yu CS et al.2001a.Intrusive activities during compression-extension tectonic conversion in the Bogda intracontinental orogen.Acta Petrologica Sinica,17 (2):187-198(in Chinese with English abstract)

    [19]

    Gu LX,Hu SX,Yu CS,Wu CZ and Yan ZF.2001b.Initiation and evolution of the Bogda subduction-torn-type rift.Acta Petrologica Sinica,17(4):585 -579 (in Chinese with English abstract)

    [20]

    Gu LX,Yang H,Tao XC,Yan ZF et al.1990. Rb-Sr geochronology of granites in the east section of the Mid-Tianshan belt and its tectonic evolution.Journal of Guilin College of Geology,10(1):49-55 (in Chinese with English abstract)

    [21]

    Gu LX,Yang H,Yan ZF,Liao JJ,and Wang JZ.1996. Geology and genesis of peraluminous granites in east Toanshan upper Paleozoic island arc belt.Chinese Journal of Geochemistry,15(1):33 -43

    [22]

    Gu LX,Zhu JL,Guo JC,Liao JJ,Yan H and Wang JZ.1995. Geology and genesis of the mafic-ultramafic complexes in the HuangshanJingerquan belt,East Xinjiang.Chinese Journal of Geochemistry.14(2):97-116

    [23]

    Guo ZJ,Ma RS,Guo LZ,Shi YS.1993. A comparative study on three ophiolitic melange belts in Eastern Xinjiang.Geological Review,39(3):236 -247 (in Chinese with English abstract)

    [24]

    Han BF,Ji JQ,Song B,Chen LH,Li ZH.2004. SHRIMP Zircon U-Pb ages of Kalatongke No.1 and Huangshandong Cu-Ni-bearing maficultramafic complexes,North Xinjiang,and geological implications.Chinese Science Bulletin,49(22):2424 -2429

    [25]

    Harris NBW,Pearce JA and Tindle AG.1986. Geochemical characteristics of collision-Zone magmatism In:Coward MP and Reis AC (eds.),Collision tectonics.Spec.Publ.Hrol.Soc.Lond.,19,67-81

    [26]

    He GQ,Li MS,Liu DQ et al.1994. Paleozoic crustal evolution and mineralization in Xinjiang of China.Urumqi and Hongkong:Xingjiang People\'s Publication House and Educational and Cultural Press LTD,1 -437 (in Chinese with English abstract)

    [27]

    Hu Shouxi,Guo Jichun,Gu Lianxing,et al.1990. Geology of the Caledonian orogenic belt and its importance to the framework of East Tianshan.Geoscience of Xinjiang,edited by The Editorial Committee of Geoscience of Xinjiang of Project 305. No.1:32-46(in Chinese with English abstract)

    [28]

    Jackson SE,Pearson NJ,Griffin WL,Belousova EA.2004. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U Pb zircon geochronology.Chemical Geology,211:47-69

    [29]

    Ji JS,Tao HX,Yang XK.1994. Geochemical Characteristics of volcanic rocks within different tectonic settings in the central part of East Tianshan,Acta Petrologica et Mineralogica,13 (4):297-304 (in Chinese with English abstract)

    [30]

    Laurent CS,Charvet J,Monie P,Shu LS.2003. Late Paleozoic strikeslip shear zones in eastern central Asia (NW China):new structural and geochronological data.Tectonics,22 (2):1009 -1032

    [31]

    Laurent CS,Charvet J,Shu LS,Ma RS,Lu HF.2002. Paleozoic late dollisional strike-slip deformation in Tianshan and Altay,Eastern Xinjiang,NW China.Terra Nova,14(4):249 -256

    [32]

    Li HQ,Chen FW,Lu YF,Yang HM,Guo J,Mei YP.2004. Zircon SHRIMP U-Pb age and strontium isotopes of Mineralized granitoids in the Sanchakou copper Polymetallic deposit,east Tianshan mountains.Acta Geoscientica sinica,25 (2):191-195 (in Chinese with English abstract)

    [33]

    Li HQ,Xie CF,Chang HL.1998. Study on Metallogenetic Chronology of Nonferrous and Precious Metallic Ore Deposits in Noyth Xinjiang,China.Beijing:Geological Publishing House,1-263

    [34]

    Li JY,Wang KZ,Li WQ,Guo HC,Song B,Wang Y,Mo SG,Zhao ZR,Pan CZ.2002. Tectonic evolution since the late Paleozoic and Mineral prospecting in Eastern Tianshan Mountains,NW China.Xinjiang Geology,22 (4):295-301 (in Chinese with English abstract)

    [35]

    Li JY,Xiao W J,Wang KZ,Sun GH,Gao LM.2003. Neoproterozoicpaleozoic tectonostratigraphy magmatic activities and tectonic evolution of eastern Xinjiang,NW China.Tectonic evolution and metallogeny of the Chinese Altay and Tianshan proceedings volume of the international symposium of the IGGP-473 project in Urumqi and Guidebook of the field excursion in Xinjiang,China:August 9-21,2003. IAGOD Guidebook Series 10:CERCAMS/NHM London,pp.31 -74

    [36]

    Li WQ,Dong FR,Zhou RH.2000. Ophiolite discovered in Kangurtag region and its characteristics.Xinjiang Geology,18(2):121 -128(in Chinese with English abstract)

    [37]

    Li XJ,Li XH.1999. Geology and metallogenesis of the Bailingshan iron deposit in Shanshan,Xinjiang.Geology and Prospecting,35(3):9-13 (in Chinese with English abstract)

    [38]

    Liu DQ,Chen YC,Wang DL,Tang YL,Zhou YH,Wang Jinliang Li HQ,Chen FW.2003. A discussion on problems related to mineralization of Tuwu Yndong Cu Mo ore field in Hami,Xinjiang.Mineral deposits,22 (4):334-344 (in Chinese with English abstract)

    [39]

    Ma RS,Shu LS and Su JQ.1997. Tectonic Evolution and Metallogeny of Eastern Tianshan Mountains.Beijing:Geological Publishing House,1 -202 (in Chinese with English abstract)

    [40]

    Ma RS,Wang CY and Ye SF.1993. Tectonic Framework and Crustal Evolution of Eastern Tianshan Mountains.Nanjing:Publishing House of Nanjing University,1 -255 (in Chinese with English abstract)

    [41]

    Maniar PD and Piccoli PM.1989. Tectonic discrimination of granitoids.Geological Society of America Bulletin,101:635 -643

    [42]

    Mao JW,Yang JM,Han CM,Wang ZL.2002. Metallogenic systems of polymetallic copper and gold deposits and related metallogenic geodynamic model in Eastern Tianshan,Xinjiang.Earth Science Journal of China University of Geosciences,27 (4):413-424 (in Chinese with English abstract)

    [43]

    Middlemost EAK.1994. Naming materials in the magma/igneous rocks system.Earth-Science Reviews,37:215-224

    [44]

    Mitchell AHG.and Garson MS.1981. Mineral Depositsand Global Tectonic Settings.London:Academic Press.1-405

    [45]

    Naldrett AJ and Cabri LJ.1976. Ultramafic and related mafic rocks:their classification and genesis with special reference to the concentration of nickel sulphides and platinum-group elements.Economic Geology,71:1131 -1158

    [46]

    Patio DAE.1999. What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas?In:Castro A,Fern ndez C,Vigneresse JL (eds),Understanding granites:Intergrating new and classical techniques.Geological Society,London,Special Publications,168:55 -75

    [47]

    Qin KZ,Fang TH,Wang SL,Zhu BQ,Feng YM,Yu HF,Xiu QY.2002. Plate tectonic division,evolution and metallogenic settings in Eastern Tianshan Mountains,NW-China.Xinjiang Geology,20(4):302 -308 (in Chinese with English abstract)

    [48]

    Qin KZ,Zhang LC,Xiao WJ,Xu XW,Yan Z,Mao JW.2003. Overview of major Au,Cu,Ni and Fe deposits and metallogenic evolution of the eastern Tianshan mountains,Northwestern China.In:Mao,Goldfarb,Setlmann,Wang,Xiao &Hart (Eds),Tectonic evolution and Metallogeny of the Chinese Altay and Tianshan Proceedings volume of the international symposium of the IGCP-473project in Urumqi and Guidebook of the Field excursion in Xinjaing,China:August 9 -21,IAGOD guidebook series 10:CERCAMS/NHM London,pp.227-248

    [49]

    Rui ZY,Wang LS,Wang YT,Liu YL.2002. Discussion on metallogenic epoch of Tuwu and Yandong porphyry copper deposits in Eastern Tianshan Mountians,Xinjiang.Mineral Deposits,21 (1):16 -22 (in Chinese with English abstract)

    [50]

    Seng r AMC,Natal in BA,and Burtman VS.1993. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia.Nature,364:209-304

    [51]

    Shu LS,Charvet J,Guo LZ,Lu HF,and Laurent-Charvet S.1999. A large-scale palaeozoic destral ductile strike-slip zone:the Aqqikkudug-Weiya zone along the Northern Margin of the Central Tianshan belt,Xinjiang,NW China.Acta Geologica Sinica,73(2):148 -162

    [52]

    Tatsumi Y and Kimura N.1991. Backarc extension versus continental breakup:petrological aspects for active rifting.Tectonophysics,197:127-137

    [53]

    Taylor SR and Mclennan SM.1981. The compostition and evolution of the continental crust:rare earth element evidence from sedimentary rocks.Phil.Trans.R.Soc.London,A301,381 -399

    [54]

    Ubatto D.2002. Zircon trace element geochemistry:Partitioning with garnet and the link between U-Pb ages and metamorphism.Chemical Geology,184:123-138

    [55]

    Vavra G,Gebauer D,Schmid R,et al.1996. Multiple zircon growth and recrystallization during polyphase late Carboniferous to Triassic metamorphism in granulites of the Ivrea Zone (Southern Alps):An ion microprobe (SHRIMP) study.Contrib.Mineral.Petrol.,122:337-358

    [56]

    Vavra G,Schmid R,Gebauer D.1999. Interanal morphology,habit and U-Th-P microanalysis of amphibolite-to-granulite facies zircons:Geochronology of the Ivrea Zone (Southern Alps).Contrib.Mineral.Petrol.,134:380-404

    [57]

    Wang BX,Li ZN,Zhao GZ,Wang FB.1989. Geochemical characteristics of granitoids in the eastern sector of the northern Tianshan mountains,Xinjiang.Acta Geologica Sinica,63 (3):237-245 (in Chinese with English abstract)

    [58]

    Wang CY,Zhu WB,Ma RS.1992. Research on characters and mechanism of metamorphism from Kusui metamorphic zone in the eastern Tianshan.Journal of Nanjing University (Natural Sciences Edition),28 (4):595-604 (in Chinese)

    [59]

    Wang LS,Li HQ,Chen YC and Liu DQ.2005. Geological feature and mineraliation epoch of Bailingshan iron deposit,Hami,Xinjiang,China.Mineral Deposits,24 (3):264-269 (in Chinese with English abstract)

    [60]

    Wareham CD,Vaughan APM,Miller IL.1997. The Wiiley Glacier complex,Antarctic peninsula:pluton growth by pulsing of granitoid magmas.Chem.Geol.,143:65 -80

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收稿日期:  2005-12-20
修回日期:  2006-04-12
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