新疆西准噶尔达拉布特蛇绿岩E-MORB型镁铁质岩的地球化学、年代学及其地质意义
Geochemistry and dating of E-MORB type mafic rocks from Dalabute ophiolite in West Junggar, Xinjiang and geological implications
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摘要: 新疆西准噶尔地区是古生代经过俯冲-增生形成的复合造山带,该地区分布有多条蛇绿岩带,其中之一的西准噶尔达拉布特蛇绿岩被认为是最大的一条蛇绿岩带,可能代表了古亚洲洋壳的残余。本文的资料显示蛇绿岩带内的镁铁质岩呈现出N-MORB、E-MORB和似OIB的地球化学特征,通过对阿克巴斯套岩体中的浅色辉长岩LA-ICP-MS锆石年龄测定,获得达拉布特蛇绿岩E-MORB型镁铁质岩的年龄为302±1.7Ma。鉴于达拉布特蛇绿岩中E-MORB和似OIB型镁铁质岩成因的复杂性,结合前人研究成果,对辉长岩锆石U-Pb年龄所代表的意义存在两种可能性:(1)E-MORB型和似OIB型镁铁质岩可能是弧后盆地扩张后期的产物,代表蛇绿岩的年龄,其表明西准噶尔地区可能晚石炭纪还有洋盆存在;(2)E-MORB型镁铁质岩是蛇绿岩消亡阶段由于扩张脊和俯冲带碰撞作用而形成的弧前海山,形成时代晚于达拉布特主体蛇绿岩,但其成因与蛇绿岩的演化密切相关。本文侵向于第二种可能性,认为新疆北部晚石炭-早二叠可能仍存在活动陆缘,俯冲作用仍然存在,扩张脊俯冲形成的板片窗效应导致地幔楔、俯冲板片和沉积物等熔融促使基性岩浆向长英质酸性岩浆转变,从而引发了二叠纪大规模玄武质岩浆底侵,导致了该时期的构造-岩浆-成矿-造山作用的发生。Abstract: The West Junggar region in northwestern China is an important part of Central Asian Orogenic Belt, which consists of successive subduction-accretion of ophiolites, island arc, oceanic ialands, seamounts, accretionary wedges in Paleozoic. A number of ophiolites or ophiolitic melanges were emplaced within this orogenic belt, Dalabute ophiolite, which is one of the largest ophiolite belts in West Junggar, represents the remnants of Paleoasian oceanic crust. Geochemically, the mafic rocks of Dalabute ophiolite display normal mid-ocean ridge basalt (N-MORB), enriched mid-ocean ridge basalt (E-MORB) and ocean island basalt (OIB) signatures. This paper reports that the LA-ICP-MS zircon U-Pb dating result for E-MORB type leucocratic gabbros from Akebasitao terrane of Dalabute ophiolite, yielding an age of 302±1.7Ma. Since the more complexity petrogenesis of E-MORB and OIB mafic rocks in ophiolites, combining previous studies, we propose two hypotheses for explanation of gabbro age: (1)E-MORB and OIB type mafic rocks were formed in late stage of back arc extension, the dating represents the formation age of the ophiolite, suggesting the Junggar ocean possibly closed after Late Carboniferous; (2) E-MORB and OIB type mafic rocks were forearc seamount in accretionary prism during the death or emplacement stage of ophiolite, which formed in response to collision of spreading center with Dulabute ophiolite subduction zone. They post-dated formation of main ophiolite sequence, but have significant tectonic implications for the origin and evolution of the Dalabute ophiolite. We favor the latter explanation and propose that there was an active margin during the Late Carboniferous-Early Permian in North Xinjiang. The important cause of tectonic-magmatic-metallogenic-orogenic climax is the subdution of spreading center, by which the large volume of continental crust increased through transfer granitic melt, which were from partial melting of accretionary wedge, subducted slab and recycled sediments triggered by underplating of mantle-derived basaltic magmas, to orogenic belt. This process may be caused by slab window effects following spreading center subduction.
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[1] Alabaster T,Pearce JA,Malpas J,The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex,Contributions to Mineralogy & Petrology,1982(03).
[2] Andersen T,Correction of common lead in U-Pb analyses that do not report 204pb,Chemical Geology,2002(1-2).
[3] Ayuso RA,Haeussler PJ,Bradley DC,Farris DW Foley NK and Wandless GA,The role of ridge subduction in determining the geochemistry and Nd-Sr-Pb isotopic evolution of the Kodiak batholith in southern Alaska,Tectonophysics,2009.
[4] Bai WJ,Yang JS,Zhou MF,Tectonic evolution of different dating ophiolites in in West Junggar,Xinjiang,Acta Petrologica Sinica,1995(zk).
[5] Benoit M,Aguillon-Robles A,Calmus T,Maury R Bellon H Cotten J Bourgois J and Michaud F,Geochemical diversity of Late Miocene volcanism in southern Baja California,Mexico:Implication of mantle and crustal sources during the opening of an asthenospheric window,Journal of Geology,2002.
[6] Bradley DC,Kusky TM,Haeussler PJ,Goldfarb RJ Miller ML Dumoulin JA Nelson SW and Karl SM,Geologic signature of Early Tertiary ridge subduction in Alaska,Geological Society of America Special Paper,2003.
[7] Buckman S,Aitchison JC,Tectonic evolution of Palaeozoic terranes in West Junggar,Xinjiang,NW China,Geological Society of London Special Publications,2004(01).
[8] Buslov MM,Fujiwara Y,Iwata K,Semakov NN,Late Paleozoic-Early Mesozoic geodynamics of Central Asia,Gondwana Research,2004(03).
[9] Buslov MM,Watanabe T,Fujiwara Y,Iwata K Smirnova LV Safonova IY Semakov NN and Kiryanova AP,Late Paleozoic faults of the Altai region,Central Asia:Tectonic pattern and model of formation,Journal of Asian Earth Sciences,2004(05).
[10] Castillo PR,Origin of the adakite-high-Nb basalt association and its implications for postsubduction magmatism in Baja California,Mexico,Geological Society of America Bulletin,2008.
[11] Chen B,Arakawa Y,Elemental and Nd-Sr isotopic geochemistry of granitoids from the West Junggar foldbelt(NW China),with implications for Phanerozoic continental growth,Geochimica et Cosmochimica Acta,2005(05).
[12] Chen B,Jahn BM,Genesis of post-collisional granitoids and basement nature of the Junggar Terrane,NW China:Nd-Sr isotope and trace element evidence,Journal of Asian Earth Sciences,2004(05).
[13] Coleman RG,Continental growth of northern China,Tectonics,1989(03).
[14] Cole RB,Nelson SW,Layer PW,Oswald PJ,Eocene volcanism above a depleted mantle slab window in southern Alaska,Geological Society of America Bulletin,2006(1-2).
[15] Cole RB,Stewart BW,Continental margin volcanism at sites of spreading ridge subduction:Examples from southern Alaska and western California,Tectonophysics,2009(1-4).
[16] Dilek Y,Collision tectonics of the Mediterranean region:Causes and consequences,Geological Society of America Special Paper,2006(01).
[17] Donnelly KE,Goldstein SL,Langmuir CH,Spiegelman M,Origin of enriched ocean ridge basalts and implications for mantle dynamics,Earth and Planetary Science Letters,2004(3-4).
[18] Feng Y,Coleman RG,Tilton G,Xiao X,Tectonic evolution of the West Junggar region,Xinjiang,China,Tectonics,1989(04).
[19] Fretzdorff S,Livermore RA,Devey CW,Leat PT and Stoffers P,Petrogenesis of the back-arc East Scotia Ridge,South Atlantic Ocean,Journal of Petrology,2002(08).
[20] Frey FA,Green DH,Roy SD,Integrated models of basalt petrogenesis:A study of quartz tholeiites to olivine melilitites from southeastern Australia utilizing geochemical and experimental petrological data,Journal of Petrology,1978(03).
[21] Frey FA,Prinz M,Ultramafic inclusions from San Carlos,Arizona:Petrologic and geochemical data bearing on their petrogenesis,Earth and Planetary Science Letters,1978(01).
[22] Frey FA,Walker N,Stakes D,Hart SR and Nielsen R,Geochemical characteristics of basaltic glasses from theamar andfamous axial valleys,Mid-Atlantic Ridge(36-37 N):Petmgenetic implications,Earth and Planetary Science Letters,1993(1-4).
[23] Gao S,Liu X,Yuan H,Hattendorf B Gunther D Chen L and Hu S,Determination of forty two major and trace elements in USGS and NIST SRM Glasses by laser ablation-inductively coupled plasmamass spectrometry,Geostandards and Geoanalytical Research,2002(02).
[24] Gao SL,He ZL,Zhou ZY,Geochemical characteristics of the Karamay granitoids and their significance in West Junggar,Xinjiang,Xinjiang Geology,2006(02).
[25] Gribble RF,Stern RJ,Bloomer SH,St ben D O\'Hearn T and Newman S,MORB mantle and subduction components interact to generate basalts in the southern Mariana Trough back-arc basin,Geochimica et Cosmochimica Acta,1996(12).
[26] Gribble RF,Stern RJ,Newman S,Bloomer SH and O\'Hearn T,Chemical and isotopic composition of lavas from the northern Mariana Trough:Implications for magmagenesis in back-arc basins,Journal of Petrology,1998(01).
[27] Hastie AR,Kerr AC,Pearce JA,Mitchell SF,Classification of altered volcanic island arc rocks using immobile trace elements:Development of the Th/Co discrimination diagram,Journal of Petrology,2007(12).
[28] Han BF,Ji JQ,Song B,Chen LH and Zhang L,Late Paleozoic vertical growth of continental crust around the Junggar Basin,Xinjiang,China(Part Ⅰ):Timing of post-collisional plutonism,Acta Petrologica Sinica,2006(05).
[29] Hao ZG,Wang XB,Geological characteristics and genetic study on ophiolites of the two types in the western Junggar,Xinjiang,Acta Petrologica et Mineralogica,1989(04).
[30] Hawkins JW,Geology of supra-subduction zones:Implications for the origin of ophiolites,Geological Society of America Special Paper,2003(0).
[31] He GQ,Liu JB,Zhang YQ,Xu X,Keramay ophiolitic melange formed during Early Paleozoic in western Junggar basin,Acta Petrologica Sinica,2007(07).
[32] Hemond C,Hofmann AW,Vlast lic I,Naurent F,Origin of MORB enrichment and relative trace element compatibilities along the Mid-Atlantic Ridge between 10° and 24° N,Geochemistry Geophysics and Geosystems,2006.
[33] Isozaki Y,Anatomy and genesis of a subduction-related orogen:A new view of geotectonic subdivision and evolution of the Japanese Islands,Island Arc,1996(03).
[34] Jahn BM,The Central Asian Orogenic Belt and growth of the continental crust in the Phanerozoic,Geological Society London Special Publications,2004(01).
[35] Jahn BM,Wang T,Litvinovsky BA,Crustal growth in the Central Asian Orogenic Belt(the Altaids):Nd isotope evidence,Geochimica et Cosmochimica Acta,2006(z.1).
[36] Jahn BM,Wu FY,Chen B,Massive granitoid generation in Central Asia:Nd isotope evidence and implication for continental growth in the Phanerozoic,Episodes,2000(02).
[37] Jiang Y,Li SZ,Zhen QZ,Li SL Feng XC and Dong FR,Chemistry character and formed environment of super-magnesium-iron ore of Dalabute,West Junnar region,Xinjiang Geology,2003(02).
[38] Juteau T,Maury RC,Juteau T,The Oceanic Crust,from Accretion to Mantle recycling,Springer-verlag,1999.
[39] Kamenetsky VS,Crawford AJ,Eggins S,Muhe R,Phenocryst and melt inclusion chemistry of near-axis seamounts,Valu Fa Ridge,Lau Basin:Insight into mantle wedge melting and the addition of subduction components,Earth and Planetary Science Letters,1997(3-4).
[40] Kwon ST,Tihon GR,Coleman RG,Feng Y,Isotopic studies bearing on the tectonics of the West Junggar region,Xinjiang,China,Tectonics,1989(04).
[41] Loat PT,Livermore RA,Millar IL,Pearce JA,Magma supply in back-arc spreading Centre Segment E2,East Scotia Ridge,Journal of Petrology,2000(06).
[42] Let M,Zhao ZD,Hou QY,Zhang HF Xu JF Chen YL Zhang BR and Liu XJ,Geochemical and Sr-Nd-Pb isotopic characteristics of the Dalabute ophiolite,Xinjiang:Comparison between the Paleo-Asian ocean and the Tethyan mantle domains,Acta Petrologica Sinica,2008(04).
[43] Li HQ,Xie CF,Chang HL,Cai H,Zhu JP Zhou S,Study on Metallogenic Chronology of the Nonferrous and Precious Metallic Ore Deposits in North Xinjiang,北京:地质出版社,1998.
[44] Liu XJ,Xu JF,Hou QY,Bai ZH and Lei M,The geochemical characteristics of Karamaili ophiohte in East Junggar,Xinjiang:Products of ridge subduction,Acta Petrologica Sinica,2007(07).
[45] Long XP,Sun M,Yuan C,Xiao WJ Chen HL Zhao YJ Cai KA and Li JL,Genesis of Carboniferous volcanic rocks in the eastern Junggar:Constraints on the closure of the Junggar Ocean,Acta Petrologica Sinica,2006(01).
[46] Ludwig RK,ISOPLOT-A plotting and regression program for radiogenic-isotope data,Version 2.96,Revision of US Geological Survey Open File Report,1998(445).
[47] Maruyama S,Pacific-type orogeny revisited:Miyashiro-type orogeny proposed,Island Arc,1997(01).
[48] Maury RC,Fourcade S,Coulon C,El Azzouzi Mh Bellon H Coutelle A Ouabadi A Semroud B Megartsi Mh Cotten J Belanteur O Louni-Hacini A Piqu A Capdevila R Hernandez J and R hault JP,Post-collisional Neogene magmatism of the Mediterranean Maghreb margin:A consequence of slab breakoff,Comptes Rendus de l\'Acad mie des Sciences Series IIA-Earth and Planetary Science,2000(03).
[49] Niu Y,Batiza R,Trace element evidence from seamounts for recycled oceanic crust in the Eastern Pacific mantle,Earth and Planetary Science Letters,1997(3-4).
[50] Niu Y,Collerson KD,Batiza R,Wendt JI and Regelous M,The origin of E-type MORB at ridges far from mantle plumes:The East Pacific Rise at 11 20\'N,Journal of Geophys Research,1999.
[51] Pearce JA,Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crest,Lithos,2008(1-4).
[52] Pearce JA,Peate DW,Tectonic implications of the composition of volcanic ARC magmas,Annual Review of Earth and Planetary Sciences,1995(01).
[53] Rudnick RL,Making continental crest,Nature,1995.
[54] Schilling JG,Thompson G,Kingsley R,Humphris S,Hotspotmigrating ridge interaction in the South Atlantic,Nature,1985(5999).
[55] Sengor AMC,Natal\'in B,Paleotectonics of Asia:Fragments of a synthesis,New York:cambridge University Press,1996.
[56] Sengor AMC,Natal\'in BA,Turkic-type orogeny and its role in the making of the continental crust,Annual Review of Earth and Planetary Sciences,1996(01).
[57] Sengor AMC,Natal\'in BA,Burtman VS,Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia,Nature,1993(6435).
[58] Shervais JW,Birth,death,and resurrection:The life cycle of suprasubduction zone ophiolites,Geochemistry Geophysics and Geosystems,2001.
[59] Shervais J,Kolesar P,Andreasen K,A field and chemical study of serpentinization-stonyford,California:Chemical flux and mass balance,International Geology Review,2005(01).
[60] Shervais JW,Schuman MMZ,Hanan BB,The Stonyford volcanic complex:A Forearc Seamount in the northern California Coast Ranges,Journal of Petrology,2005(10).
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