中天山地块南缘两类混合岩的成因及其地质意义
|
摘要
中天山地块是位于中亚造山带西南缘的西天山造山带的重要组成块体,其基底演化和构造亲缘性对恢复西天山的增生造山方式和大地构造格局具有重要意义。混合岩在中天山地块的高级变质地体中广泛分布,是揭示中天山地块基底演化和构造属性的窗口。本文通过开展锆石U-Pb年代学和Hf同位素及岩石地球化学研究,确定了中天山地块南缘乌瓦门杂岩的两类条带状混合岩的原岩性质和形成时代以及混合岩化作用时代和成因机制。第一类条带状混合岩的原岩为中基性岩屑砂岩,混合岩化时代为～1. 8Ga,是在同期角闪岩相变质过程中通过变质分异形成的。第二类条带状混合岩的古成体包括黑云角闪斜长片麻岩和黑云斜长角闪片麻岩,原岩均形成于～2. 5Ga,并叠加～1. 8Ga角闪岩相变质作用,是洋陆俯冲背景下由俯冲洋壳或岩石圈地幔部分熔融形成。侵入古成体的变基性岩墙形成于～1. 72Ga,具有Fe-Ti玄武岩的地球化学特征,起源于后碰撞伸展背景下的软流圈地幔。该类混合岩的浅色体同时穿插古成体和变基性岩墙,呈现突变的野外接触关系,与区域内约787～785Ma混合岩化同期,即混合岩化作用是外来岩浆注入的结果,可能是造山带垮塌引发地壳深熔作用的产物。乌瓦门杂岩记录的～2. 5Ga岩浆活动、～1. 8Ga变质作用和～790Ma混合岩化作用可以和塔里木北缘进行对比,暗示中天山地块是一个具有确切新太古代-古元古代结晶基底的微陆块,并且和塔里木克拉通存在构造亲缘性。
The Central Tianshan Block is a major constituent of the Paleozoic Western Tianshan Orogen in the southwestern Central Asian Orogenic Belt,and its geological evolution and tectonic affinity is essential to reconstruction of the architectural framework and subduction-accretion processes of the Western Tianshan Orogen. The ubiquitous migmatites in high-grade metamorphic terranes provide an excellent window to the tectonic evolution and affinity of the crustal basement of the Central Tianshan Block. Here we present zircon U-Pb-Hf isotopic and whole-rock geochemical data for two contrasting migmatites from the Wuwamen complex in the southern Central Tianshan Block. The first type of stromatic migmatite with an intermediate-mafic greywacke protolith underwent migmatization at ca. 1. 8 Ga,resulted from metamorphic differentiation associated with the coeval amphibolite facies metamorphic event. The paleosomes of the second type of stromatic migmatite are composed of interlayered orthogneisses with protolith formation ages at ca. 2. 5 Ga and an amphibolite facies metamorphic overprint at ca. 1. 8 Ga. Geochemical data reveal that they were derived from partial melting of subducted oceanic crust or lithospheric mantle in an oceanic subduction setting. The meta-mafic dykes intruding the orthogneisses were formed at ca. 1. 72 Ga and display geochemical affinity to Fe-Ti basalts,which are interpreted to be derived from partial melting of the asthenospheric mantle in a post-collisional setting. The leucosomes crosscut the orthogneisses and meta-mafic dykes with a sharp contact relationship,suggesting that migmatization was resulted from injection of external partial melts probably induced by anataxis during orogenic collapse. The ～ 2. 5 Ga magmatism, ～ 1. 8 Ga metamorphism and ～ 790 Ma migmatization recorded by the Wuwamen complex are comparable to those events in the northern Tarim Craton,and thus we conclude that the Central Tianshan Block is a microcontinent with a Neoarchean-Paleoproterozoic basement and has a close affinity with the Tarim Craton.
The Central Tianshan Block is a major constituent of the Paleozoic Western Tianshan Orogen in the southwestern Central Asian Orogenic Belt,and its geological evolution and tectonic affinity is essential to reconstruction of the architectural framework and subduction-accretion processes of the Western Tianshan Orogen. The ubiquitous migmatites in high-grade metamorphic terranes provide an excellent window to the tectonic evolution and affinity of the crustal basement of the Central Tianshan Block. Here we present zircon U-Pb-Hf isotopic and whole-rock geochemical data for two contrasting migmatites from the Wuwamen complex in the southern Central Tianshan Block. The first type of stromatic migmatite with an intermediate-mafic greywacke protolith underwent migmatization at ca. 1. 8 Ga,resulted from metamorphic differentiation associated with the coeval amphibolite facies metamorphic event. The paleosomes of the second type of stromatic migmatite are composed of interlayered orthogneisses with protolith formation ages at ca. 2. 5 Ga and an amphibolite facies metamorphic overprint at ca. 1. 8 Ga. Geochemical data reveal that they were derived from partial melting of subducted oceanic crust or lithospheric mantle in an oceanic subduction setting. The meta-mafic dykes intruding the orthogneisses were formed at ca. 1. 72 Ga and display geochemical affinity to Fe-Ti basalts,which are interpreted to be derived from partial melting of the asthenospheric mantle in a post-collisional setting. The leucosomes crosscut the orthogneisses and meta-mafic dykes with a sharp contact relationship,suggesting that migmatization was resulted from injection of external partial melts probably induced by anataxis during orogenic collapse. The ～ 2. 5 Ga magmatism, ～ 1. 8 Ga metamorphism and ～ 790 Ma migmatization recorded by the Wuwamen complex are comparable to those events in the northern Tarim Craton,and thus we conclude that the Central Tianshan Block is a microcontinent with a Neoarchean-Paleoproterozoic basement and has a close affinity with the Tarim Craton.
引文
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report204Pb.Chemical Geology,192(1-2):59-79
Bouvier A,Vervoort JD and Patchett PJ.2008.The Lu-Hf and Sm-Nd isotopic composition of CHUR:Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets.Earth and Planetary Science Letters,273(1-2):48-57
Brown M.1994.The generation,segregation,ascent and emplacement of granite magma:The migmatite-to-crustally-derived granite connection in thickened orogens.Earth-Science Reviews,36(1-2):83-130
Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomy Region.1993.Regional Geology of Xinjiang Uygur Autonomy Region.Beijing:Geological Publishing House(in Chinese)
Cheng YQ.1987.On migmatites and migmatization-Half a century’s recollection of certain related problems.Bulletin of the Chinese Academy of Geological Sciences,16:5-19(in Chinese with English abstract)
Condie KC,Belousova E,Griffin WL and Sircombe KN.2009.Granitoid events in space and time:Constraints from igneous and detrital zircon age spectra.Gondwana Research,15(3-4):228-242
Corfu F,Hanchar JM,Hoskin PWO and Kinny P.2003.Atlas of zircon textures.Reviews in Mineralogy and Geochemistry,53(1):469-500
Fenner CN.1929.The crystallization of basalts.American Journal of Science,18(105):225-253
Foster DA,Schafer C,Fanning CM and Hyndman DW.2001.Relationships between crustal partial melting,plutonism,orogeny,and exhumation:Idaho-Bitterroot batholith.Tectonophysics,342(3-4):313-350
Frey FA,Green DH and Roy SD.1978.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,19(3):463-513
Gao J,He GQ,Li MS,Xiao XC,Tang YQ,Wang J and Zhao M.1995.The mineralogy,petrology,metamorphic PTDt trajectory and exhumation mechanism of blueschists,South Tianshan,northwestern China.Tectonophysics,250(1-3):151-168
Gao J,Li MS,Xiao XC,Tang YQ and He GQ.1998.Paleozoic tectonic evolution of the Tianshan Orogen,northwestern China.Tectonophysics,287(1-4):213-231
Gao J,Long LL,Klemd R,Qian Q,Liu DY,Xiong XM,Su W,Liu W,Wang YT and Yang FQ.2009.Tectonic evolution of the South Tianshan orogen and adjacent regions,NW China:Geochemical and age constraints of granitoid rocks.International Journal of Earth Sciences,98(6):1221-1238
Gao J,Qian Q,Long LL,Zhang X,Li JL and Su W.2009.Accretionary orogenic process of Western Tianshan,China.Geological Bulletin of China,28(12):1804-1816(in Chinese with English abstract)
Gao J,Klemd R,Qian Q,Zhang X,Li JL,Jiang T and Yang YQ.2011.The collision between the Yili and Tarim blocks of the southwestern Altaids:Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen.Tectonophysics,499(1-4):118-131
Gao J,Wang XS,Klemd R,Jiang T,Qian Q,Mu LX and Ma YZ.2015.Record of assembly and breakup of Rodinia in the southwestern Altaids:Evidence from Neoproterozoic magmatism in the Chinese Western Tianshan Orogen.Journal of Asian Earth Sciences,113:173-193
Gao J,Zhu MT,Wang XS,Hong T,Li GM,Li JL,Xiao WJ,Qin KZ,Zeng QD,Shen P,Xu XW,Zhang ZC,Zhou JB,Lai Y,Zhang XH,Sun JG,Wan B and Wang B.2019.Large-scale porphyry-type mineralization in the Central Asian metallogenic domain:Tectonic background,fluid feature and metallogenic deep dynamic mechanism.Acta Geologica Sinica,93(1):24-71(in Chinese with English abstract)
Ge RF,Zhu WB,Wu HL,Zheng BH,Zhu XQ and He JW.2012.The Paleozoic northern margin of the Tarim Craton:Passive or active?Lithos,142-143:1-15
Ge RF,Zhu WB,Wu HL,He JW and Zheng BH.2013a.Zircon U-Pb ages and Lu-Hf isotopes of Paleoproterozoic metasedimentary rocks in the Korla Complex,NW China:Implications for metamorphic zircon formation and geological evolution of the Tarim Craton.Precambrian Research,231:1-18
Ge RF,Zhu WB,Wu HL,Zheng BH and He JW.2013b.Timing and mechanisms of multiple episodes of migmatization in the Korla Complex,northern Tarim Craton,NW China:Constraints from zircon U-Pb-Lu-Hf isotopes and implications for crustal growth.Precambrian Research,231:136-156
Ge RF,Zhu WB,Wilde SA,Wu HL,He JW and Zheng BH.2014a.Archean magmatism and crustal evolution in the northern Tarim Craton:Insights from zircon U-Pb-Hf-O isotopes and geochemistry of~2.7Ga orthogneiss and amphibolite in the Korla Complex.Precambrian Research,252:145-165
Ge RF,Zhu WB,Wilde SA,He JW,Cui X,Wang X and Zheng BH.2014b.Neoproterozoic to Paleozoic long-lived accretionary orogeny in the northern Tarim Craton.Tectonics,33(3):302-329
Ge RF,Zhu WB and Wilde SA.2016.Mid-Neoproterozoic(ca.830~800Ma)metamorphic P-T paths link Tarim to the circum-Rodinia subduction-accretion system.Tectonics,35(6):1465-1488
Gerdes A and Zeh A.2009.Zircon formation versus zircon alteration:New insights from combined U-Pb and Lu-Hf in-situ LA-ICP-MSanalyses,and consequences for the interpretation of Archean zircon from the Central Zone of the Limpopo Belt.Chemical Geology,261(3-4):230-243
Griffin WL,Belousova EA,Shee SR,Pearson NJ and O’Reilly SY.2004.Archean crustal evolution in the northern Yilgarn Craton:U-Pb and Hf-isotope evidence from detrital zircons.Precambrian Research,131(3-4):231-282
Han YG,Zhao GC,Sun M,Eizenh9fer PR,Hou WZ,Zhang XR,Liu DX,Wang B and Zhang GW.2015.Paleozoic accretionary orogenesis in the Paleo-Asian Ocean:Insights from detrital zircons from Silurian to Carboniferous strata at the northwestern margin of the Tarim Craton.Tectonics,34(2):334-351
Harper GD.2003.Fe-Ti basalts and propagating-rift tectonics in the Josephine ophiolite.Geological Society of America Bulletin,115(7):771-787
Hawkesworth C,Cawood P,Kemp T,Storey C and Dhuime B.2009.Amatter of preservation.Science,323(5910):49-50
Hawkesworth CJ,Gallagher K,Hergt JM and Mc Dermott F.1993.Mantle and slab contributions in arc magmas.Annual Review of Earth and Planetary Sciences,21(1):175-204
He ZY,Zhang ZM,Zong KQ,Wang W and Santosh M.2012.Neoproterozoic granulites from the northeastern margin of the Tarim Craton:Petrology,zircon U-Pb ages and implications for the Rodinia assembly.Precambrian Research,212-213:21-33
He ZY,Klemd R,Zhang ZM,Zong KQ,Sun LX,Tian ZL and Huang BT.2015.Mesoproterozoic continental arc magmatism and crustal growth in the eastern Central Tianshan Arc Terrane of the southern Central Asian Orogenic Belt:Geochronological and geochemical evidence.Lithos,236-237:74-89
He ZY,Wang B,Zhong LL and Zhu XY.2018a.Crustal evolution of the Central Tianshan Block:Insights from zircon U-Pb isotopic and structural data from meta-sedimentary and meta-igneous rocks along the Wulasitai-Wulanmoren shear zone.Precambrian Research,314:111-128
He ZY,Klemd R,Yan LL and Zhang ZM.2018b.The origin and crustal evolution of microcontinents in the Beishan orogen of the southern Central Asian Orogenic Belt.Earth-Science Reviews,185:1-14
Hu AQ,Zhang GX,Zhang QF and Chen YB.1998.Constraints on the age of basement and crustal growth in Tianshan Orogen by Nd isotopic composition.Science in China(Series D),41(6):648-657
Hu AQ,Wei GJ,Jahn BM,Zhang JB,Deng WF and Chen LL.2010.Formation of the 0.9Ga Neoproterozoic granitoids in the Tianshan Orogen,NW China:Constraints from the SHRIMP zircon age determination and its tectonic significance.Geochimica,39(3):197-212(in Chinese with English abstract)
Huang H,Zhang ZC,Santosh M,Zhang DY,Zhao ZD and Liu JL.2013.Early Paleozoic tectonic evolution of the South Tianshan collisional belt:Evidence from geochemistry and zircon U-Pb geochronology of the Tie’reke monzonite pluton,Northwest China.The Journal of Geology,121(4):401-424
Huang ZY,Long XP,Kr9ner A,Yuan C,Wang YJ,Chen B and Zhang YY.2015.Neoproterozoic granitic gneisses in the Chinese Central Tianshan Block:Implications for tectonic affinity and Precambrian crustal evolution.Precambrian Research,269:73-89
Huang ZY,Long XP,Yuan C,Sun M,Wang YJ,Zhang YY and Chen B.2016.Detrital zircons from Neoproterozoic sedimentary rocks in the Yili Block:Constraints on the affinity of microcontinents in the southern Central Asian Orogenic Belt.Gondwana Research,37:39-52
Huang ZY,Long XP,Wang XC,Zhang YY,Du L,Yuan C and Xiao WJ.2017.Precambrian evolution of the Chinese Central Tianshan Block:Constraints on its tectonic affinity to the Tarim Craton and responses to supercontinental cycles.Precambrian Research,295:24-37
Irvine TN and Baragar WRA.1971.A guide to the chemical classification of the common volcanic rocks.Canadian Journal of Earth Sciences,8(5):523-548
Jiang T,Gao J,Klemd R,Qian Q,Zhang X,Xiong XM,Wang XS,Tan Z and Chen BX.2014.Paleozoic ophiolitic mélanges from the South Tianshan Orogen,NW China:Geological,geochemical and geochronological implications for the geodynamic setting.Tectonophysics,612-613:106-127
Johannes W and Gupta LN.1982.Origin and evolution of a migmatite.Contributions to Mineralogy and Petrology,79(2):114-123
Johannes W,Holtz F and M9ller P.1995.REE distribution in some layered migmatites:Constraints on their petrogenesis.Lithos,35(3-4):139-152
Johannes W,Ehlers C,Kriegsman LM and Mengel K.2003.The link between migmatites and S-type granites in the Turku area,southern Finland.Lithos,68(3-4):69-90
Kelley KA and Cottrell E.2009.Water and the oxidation state of subduction zone magmas.Science,325(5940):605-607
Kriegsman LM.2001.Partial melting,partial melt extraction and partial back reaction in anatectic migmatites.Lithos,56(1):75-96
Kr9ner A,Windley BF,Badarch G,Tomurtogoo O,Hegner E,Jahn BM,Gruschka S,Khain EV,Demoux A and Wingate MTD.2007.Accretionary growth and crust formation in the Central Asian Orogenic Belt and comparison with the Arabian-Nubian shield.Geological Society of America Memoirs,200:181-209
Kr9ner A,Alexeiev DV,Rojas-Agramonte Y,Hegner E,Wong J,Xia X,Belousova E,Mikolaichuk AV,Seltmann R,Liu DY and Kiselev VV.2013.Mesoproterozoic(Grenville-age)terranes in the Kyrgyz North Tianshan:Zircon ages and Nd-Hf isotopic constraints on the origin and evolution of basement blocks in the southern Central Asian Orogen.Gondwana Research,23(1):272-295
Kr9ner A,Alexeiev DV,Kovach VP,Rojas-Agramonte Y,Tretyakov AA,Mikolaichuk AV,Xie H and Sobel ER.2017a.Zircon ages,geochemistry and Nd isotopic systematics for the Palaeoproterozoic 2.3~1.8Ga Kuilyu Complex,East Kyrgyzstan:The oldest continental basement fragment in the Tianshan orogenic belt.Journal of Asian Earth Sciences,135:122-135
Kr9ner A,Kovach V,Alexeiev D,Wang KL,Wong J,Degtyarev K and Kozakov I.2017b.No excessive crustal growth in the Central Asian Orogenic Belt:Further evidence from field relationships and isotopic data.Gondwana Research,50:135-166
Kruckenberg SC,Vanderhaeghe O,FerréEC,Teyssier C and Whitney DL.2011.Flow of partially molten crust and the internal dynamics of a migmatite dome,Naxos,Greece.Tectonics,30(3):TC3001
Li Q and Zhang LF.2004.The P-T path and geological significance of low-pressure granulite-facies metamorphism in Muzhaerte,Southwest Tianshan.Acta Petrologica Sinica,20(3):583-594(in Chinese with English abstract)
Li XH,Liu Y,Li QL,Guo CH and Chamberlain KR.2009.Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization.Geochemistry,Geophysics,Geosystems,10(4):Q04010
Long LL,Gao J,Klemd R,Beier C,Qian Q,Zhang X,Wang JB and Jiang T.2011a.Geochemical and geochronological studies of granitoid rocks from the Western Tianshan Orogen:Implications for continental growth in the southwestern Central Asian Orogenic Belt.Lithos,126(3-4):321-340
Long XP,Yuan C,Sun M,Kr9ner A,Zhao GC,Wilde S and Hu AQ.2011b.Reworking of the Tarim Craton by underplating of mantle plume-derived magmas:Evidence from Neoproterozoic granitoids in the Kuluketage area,NW China.Precambrian Research,187(1-2):1-14
Long XP and Huang ZY.2017.Tectonic affinities of microcontinents in the Central Asian Orogenic Belt:A case study of the Chinese Tianshan orogenic belt.Bulletin of Mineralogy,Petrology and Geochemistry,36(5):771-785(in Chinese with English abstract)
Ludwig KR.2003.User’s manual for Isoplot 3.00:A geochronological toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication,4:1-70
Luo FZ.1989.On Precambrian in mid-Tianshan uplift(metamorphic)zone.Xinjiang Geology,7(4):24-33(in Chinese with English abstract)
Ma XX,Shu LS,Santosh M and Li JY.2012a.Detrital zircon U-Pb geochronology and Hf isotope data from Central Tianshan suggesting a link with the Tarim Block:Implications on Proterozoic supercontinent history.Precambrian Research,206-207:1-16
Ma XX,Shu LS,Jahn BM,Zhu WB and Faure M.2012b.Precambrian tectonic evolution of Central Tianshan,NW China:Constraints from U-Pb dating and in situ Hf isotopic analysis of detrital zircons.Precambrian Research,222-223:450-473
Ma XX,Shu LS,Santosh M and Li JY.2013a.Paleoproterozoic collisional orogeny in Central Tianshan:Assembling the Tarim Block within the Columbia supercontinent.Precambrian Research,228:1-19
Ma XX,Shu LS,Santosh M and Li JY.2013b.Petrogenesis and tectonic significance of an Early Palaeozoic mafic-intermediate suite of rocks from the Central Tianshan,Northwest China.International Geology Review,55(5):548-573
Martin H,Smithies RH,Rapp R,Moyen JF and Champion D.2005.An overview of adakite,tonalite-trondhjemite-granodiorite(TTG),and sanukitoid:Relationships and some implications for crustal evolution.Lithos,79(1-2):1-24
Martin LAJ,Duchêne S,Deloule E and Vanderhaeghe O.2008.Mobility of trace elements and oxygen in zircon during metamorphism:Consequences for geochemical tracing.Earth and Planetary Science Letters,267(1-2):161-174
Mehnert KR.1968.Migmatites and the Origin of Granitic Rocks.Amsterdam:Elsevier
Meschede M.1986.A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Ydiagram.Chemical Geology,56(3-4):207-218
Moyen JF and Martin H.2012.Forty years of TTG research.Lithos,148:312-336
Pearce JA.2008.Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust.Lithos,100(1-4):14-48
Peng P,Zhai MG,Zhang HF,Zhao TP and Ni ZY.2004.Geochemistry and geological significance of the 1.8Ga mafic dyke swarms in the North China Craton:An example from the juncture of Shanxi,Hebei and Inner Mongolia.Acta Petrologica Sinica,20(3):439-456(in Chinese with English abstract)
Prouteau G,Scaillet B,Pichavant M and Maury R.2001.Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust.Nature,410(6825):197-200
Qian Q,Gao J,Klemd R,He GQ,Song B,Liu DY and Xu RH.2009.Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen:Constraints from SHRIMP zircon U-Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate,NW China.International Journal of Earth Sciences,98(3):551-569
Rojas-Agramonte Y,Herwartz D,García-Casco A,Kr9ner A,Alexeiev DV,Klemd R,Buhre S and Barth M.2013.Early Palaeozoic deep subduction of continental crust in the Kyrgyz North Tianshan:Evidence from Lu-Hf garnet geochronology and petrology of mafic dikes.Contributions to Mineralogy and Petrology,166(2):525-543
Rollinson HR.2014.Using Geochemical Data:Evaluation,Presentation,Interpretation.London:Routledge,1-351
Sawyer EW and Robin PYF.1986.The subsolidus segregation of layerparallel quartz-feldspar veins in greenschist to upper amphibolite facies metasediments.Journal of Metamorphic Geology,4(3):237-260
Sawyer EW.1996.Melt segregation and magma flow in migmatites:Implications for the generation of granite magmas.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,87(1-2):85-94
Sawyer EW.2008.Atlas of Migmatites.The Canadian Mineralogist,Special Publication 9.Ottawa:NRC Research Press,1-371
Sclar CB.1965.Layered mylonites and the processes of metamorphic differentiation.GSA Bulletin,76(5):611-612
Sederholm JJ.1907.Om granit och gneis deras uppkomst:Upptrdande och utbredning inom urberget i Fennos-kandia.Bulletin de la Commission geologique de Finlande,23
S9derlund U,Patchett PJ,Vervoort JD and Isachsen CE.2004.The176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions.Earth and Planetary Science Letters,219(3-4):311-324
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basin.Geological Society,London,Special Publications,42(1):313-345
Thy P,Lesher CE and Tegner C.2009.The Skaergaard liquid line of descent revisited.Contributions to Mineralogy and Petrology,157(6):735-747
Turner FJ.1941.The development of pseudo-stratification by metamorphic differentiation in the schists of Otago,New Zealand.American Journal of Science,239(1):1-16
Vervoort JD and Blichert-Toft J.1999.Evolution of the depleted mantle:Hf isotope evidence from juvenile rocks through time.Geochimica et Cosmochimica Acta,63(3-4):533-556
Wan B,Windley BF,Xiao WJ,Feng JY and Zhang JE.2015.Paleoproterozoic high-pressure metamorphism in the northern North China Craton and implications for the Nuna supercontinent.Nature Communications,6:8344
Wang B,Faure M,Cluzel D,Shu LS,Charvet J,Meffre S and Ma Q.2006.Late Paleozoic tectonic evolution of the northern West Chinese Tianshan belt.Geodinamica Acta,19(3-4):237-247
Wang B,Shu LS,Faure M,Cluzel D and Charvet J.2007.Paleozoic tectonism and magmatism of Kekesu-Qiongkushitai section in southwestern Chinese Tianshan and their constraints on the age of the orogeny.Acta Petrologica Sinica,23(6):1354-1368(in Chinese with English abstract)
Wang B,Shu LS,Faure M,Jahn BM,Cluzel D,Charvet J,Chung SLand Meffre S.2011.Paleozoic tectonics of the southern Chinese Tianshan:Insights from structural,chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China).Tectonophysics,497(1-4):85-104
Wang B,Jahn BM,Shu LS,Li KS,Chung SL and Liu DY.2012.Middle-Late Ordovician arc-type plutonism in the NW Chinese Tianshan:Implication for the accretion of the Kazakhstan continent in Central Asia.Journal of Asian Earth Sciences,49:40-53
Wang B,Liu HS,Shu LS,Jahn BM,Chung SL,Zhai YZ and Liu DY.2014a.Early Neoproterozoic crustal evolution in northern Yili Block:Insights from migmatite,orthogneiss and leucogranite of the Wenquan metamorphic complex in the NW Chinese Tianshan.Precambrian Research,242:58-81
Wang B,Zhai YZ,Kapp P,de Jong K,Zhong LL,Liu HS,Ma YZ,Gong HJ and Geng HY.2018c.Accretionary tectonics of back-arc oceanic basins in the South Tianshan:Insights from structural,geochronological,and geochemical studies of the Wuwamen ophiolite mélange.Geological Society of America Bulletin,130(1-2):284-306
Wang XS,Gao J,Klemd R,Jiang T,Li JL,Zhang X,Tan Z,Li L and Zhu ZX.2014b.Geochemistry and geochronology of the Precambrian high-grade metamorphic complex in the southern Central Tianshan ophiolitic mélange,NW China.Precambrian Research,254:129-148
Wang XS,Gao J,Klemd R,Jiang T,Zhai QG,Xiao XC and Liang XQ.2015.Early Neoproterozoic multiple arc-back-arc system formation during subduction-accretion processes between the Yangtze and Cathaysia blocks:New constraints from the supra-subduction zone NE Jiangxi ophiolite(South China).Lithos,236-237:90-105
Wang XS,Gao J,Klemd R,Jiang T,Li JL,Zhang X and Xue SC.2017.The Central Tianshan Block:A microcontinent with a Neoarchean-Paleoproterozoic basement in the southwestern Central Asian Orogenic Belt.Precambrian Research,295:130-150
Wang XS,Klemd R,Gao J,Jiang T,Li JL and Xue SC.2018a.Final assembly of the southwestern Central Asian Orogenic Belt as constrained by the evolution of the South Tianshan Orogen:Links with Gondwana and Pangea.Journal of Geophysical Research:Solid Earth,123(9):7361-7388
Wang XS,Zhang X,Gao J,Li JL,Jiang T and Xue SC.2018b.A slab break-off model for the submarine volcanic-hosted iron mineralization in the Chinese Western Tianshan:Insights from Paleozoic subduction-related to post-collisional magmatism.Ore Geology Reviews,92:144-160
Wiedenbeck M,AlléP,Corfu F,Griffin WL,Meier M,Oberli F,von Quadt A,Roddick JC and Spiegel W.1995.Three natural zircon standards for U-Th-Pb,Lu-Hf,trace element and REE analyses.Geostandards Newsletter,19(1):1-23
Wilhem C,Windley BF and Stampfli GM.2012.The Altaids of Central Asia:A tectonic and evolutionary innovative review.Earth-Science Reviews,113(3-4):303-341
Winchester JA and Floyd PA.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325-343
Windley BF,Alexeiev D,Xiao WJ,Kr9ner A and Badarch G.2007.Tectonic models for accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164(1):31-47
Wood DA.1980.The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province.Earth and Planetary Science Letters,50(1):11-30
Wu FY,Yang YH,Xie LW,Yang JH and Xu P.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1-2):105-126
Xia B,Zhang LF and Bader T.2014.Zircon U-Pb ages and Hf isotopic analyses of migmatite from the‘paired metamorphic belt’in Chinese SW Tianshan:Constraints on partial melting associated with orogeny.Lithos,192-195:158-179
Xiao WJ,Windley BF,Yuan C,Sun M,Han CM,Lin SF,Chen HL,Yan QR,Liu DY,Qin KZ,Li JL and Sun S.2009.Paleozoic multiple subduction-accretion processes of the southern Altaids.American Journal of Science,309(3):221-270
Xiao WJ,Windley BF,Allen MB and Han CM.2013.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage.Gondwana Research,23(4):1316-1341
Xiao WJ,Windley BF,Sun S,Li JL,Huang BC,Han CM,Yuan C,Sun M and Chen HL.2015.A tale of amalgamation of three PermoTriassic collage systems in Central Asia:Oroclines,sutures,and terminal accretion.Annual Review of Earth and Planetary Sciences,43(1):477-507
Xu YG,Mei HJ,Xu JF,Huang XL,Wang YJ and Chung SL.2003.Origin of two differentiation trends in the Emeishan flood basalts.Chinese Science Bulletin,48(4):390-394
Yang XS,Jin ZM and Ma J.2005.Anatexis in Himalayan crust:Evidence from geochemical and chronological investigations of Higher Himalayan Crystallines.Science in China(Series D),48(9):1347-1356
Zhang CL,Li XH,Li ZX,Lu SN,Ye HM and Li HM.2007.Neoproterozoic ultramafic-mafic-carbonatite complex and granitoids in Quruqtagh of northeastern Tarim Block,western China:Geochronology,geochemistry and tectonic implications.Precambrian Research,152(3-4):149-169
Zhang CL,Li HK and Wang HY.2012.A review on Precambrian tectonic evolution of Tarim Block:Possibility of interaction between Neoproterozoic plate subduction and mantle plume.Geological Review,58(5):923-936(in Chinese with English abstract)
Zhang J,Zhang CL,Li HK,Ye XT,Geng JZ and Zhou HY.2014.Revisit to time and tectonic environment of the Aksu blueschist terrane in northern Tarim,NW China:New evidence from zircon U-Pb age and Hf isotope.Acta Petrologica Sinica,30(11):3357-3365(in Chinese with English abstract)
Zhang X,Klemd R,Gao J,Dong LH,Wang XS,Haase K,Jiang T and Qian Q.2015.Metallogenesis of the Zhibo and Chagangnuoer volcanic iron oxide deposits in the Awulale Iron Metallogenic Belt,Western Tianshan orogen,China.Journal of Asian Earth Sciences,113:151-172
Zhao GC,Cawood PA,Wilde SA and Sun M.2002.Review of global2.1~1.8Ga orogens:Implications for a pre-Rodinia supercontinent.Earth-Science Reviews,59(1-4):125-162
Zhong LL,Wang B,Shu LS,Liu HS,Mu LX,Ma YZ and Zhai YZ.2015.Structural overprints of Early Paleozoic arc-related intrusive rocks in the Chinese Central Tianshan:Implications for Paleozoic accretionary tectonics in SW Central Asian Orogenic Belts.Journal of Asian Earth Sciences,113:194-217
Zhu YF,Zhou J,Song B,Zhang LF and Guo X.2006.Age of the“Dahalajunshan”Formation in Xinjiang and its disintegration.Geology in China,33(3):487-497(in Chinese with English abstract)
程裕淇．1987．有关混合岩和混合岩化作用的一些问题---对半个世纪以来某些基本认识的回顾．中国地质科学院院报，16:5-19
高俊，钱青，龙灵利，张喜，李继磊，苏文．2009．西天山的增生造山过程．地质通报，28(12):1804-1816
高俊，朱明田，王信水，洪涛，李光明，李继磊，肖文交，秦克章，曾庆栋，申萍，徐兴旺，张招崇，周建波，赖勇，张晓晖，孙景贵，万博，王博．2019．中亚成矿域斑岩大规模成矿特征:大地构造背景、流体作用与成矿深部动力学机制．地质学报，93(1):24-71
胡霭琴，韦刚健，江博明，张积斌，邓文峰，陈林丽．2010．天山0.9Ga新元古代花岗岩SHRIMP锆石U-Pb年龄及其构造意义．地球化学，39(3):197-212
李强，张立飞．2004．新疆西南天山木扎尔特一带低压麻粒岩相变质作用P-T轨迹及其地质意义．岩石学报，20(3):583-594
龙晓平，黄宗莹．2017．中亚造山带内微陆块的起源---以中国天山造山带研究为例．矿物岩石地球化学通报，36(5):771-785
罗发祚．1989．对中天山隆起(变质)带前寒武系的探讨．新疆地质，7(4):24-33
彭澎，翟明国，张华锋，赵太平，倪志耀．2004．华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例．岩石学报，20(3):439-456
王博，舒良树，Faure M,Cluzel D,Charvet J.2007．科克苏-穹库什太古生代构造-岩浆作用及其对西南天山造山时代的约束．岩石学报，23(6):1354-1368
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
张传林，李怀坤，王洪燕．2012．塔里木地块前寒武纪地质研究进展评述．地质论评，58(5):923-936
张健，张传林，李怀坤，叶现韬，耿建珍，周红英．2014．再论塔里木北缘阿克苏蓝片岩的时代和成因环境:来自锆石U-Pb年龄、Hf同位素的新证据．岩石学报，30(11):3357-3365
朱永峰，周晶，宋彪，张立飞，郭璇．2006．新疆“大哈拉军山组”火山岩的形成时代问题及其解体方案．中国地质，33(3):487-497
Bouvier A,Vervoort JD and Patchett PJ.2008.The Lu-Hf and Sm-Nd isotopic composition of CHUR:Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets.Earth and Planetary Science Letters,273(1-2):48-57
Brown M.1994.The generation,segregation,ascent and emplacement of granite magma:The migmatite-to-crustally-derived granite connection in thickened orogens.Earth-Science Reviews,36(1-2):83-130
Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomy Region.1993.Regional Geology of Xinjiang Uygur Autonomy Region.Beijing:Geological Publishing House(in Chinese)
Cheng YQ.1987.On migmatites and migmatization-Half a century’s recollection of certain related problems.Bulletin of the Chinese Academy of Geological Sciences,16:5-19(in Chinese with English abstract)
Condie KC,Belousova E,Griffin WL and Sircombe KN.2009.Granitoid events in space and time:Constraints from igneous and detrital zircon age spectra.Gondwana Research,15(3-4):228-242
Corfu F,Hanchar JM,Hoskin PWO and Kinny P.2003.Atlas of zircon textures.Reviews in Mineralogy and Geochemistry,53(1):469-500
Fenner CN.1929.The crystallization of basalts.American Journal of Science,18(105):225-253
Foster DA,Schafer C,Fanning CM and Hyndman DW.2001.Relationships between crustal partial melting,plutonism,orogeny,and exhumation:Idaho-Bitterroot batholith.Tectonophysics,342(3-4):313-350
Frey FA,Green DH and Roy SD.1978.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,19(3):463-513
Gao J,He GQ,Li MS,Xiao XC,Tang YQ,Wang J and Zhao M.1995.The mineralogy,petrology,metamorphic PTDt trajectory and exhumation mechanism of blueschists,South Tianshan,northwestern China.Tectonophysics,250(1-3):151-168
Gao J,Li MS,Xiao XC,Tang YQ and He GQ.1998.Paleozoic tectonic evolution of the Tianshan Orogen,northwestern China.Tectonophysics,287(1-4):213-231
Gao J,Long LL,Klemd R,Qian Q,Liu DY,Xiong XM,Su W,Liu W,Wang YT and Yang FQ.2009.Tectonic evolution of the South Tianshan orogen and adjacent regions,NW China:Geochemical and age constraints of granitoid rocks.International Journal of Earth Sciences,98(6):1221-1238
Gao J,Qian Q,Long LL,Zhang X,Li JL and Su W.2009.Accretionary orogenic process of Western Tianshan,China.Geological Bulletin of China,28(12):1804-1816(in Chinese with English abstract)
Gao J,Klemd R,Qian Q,Zhang X,Li JL,Jiang T and Yang YQ.2011.The collision between the Yili and Tarim blocks of the southwestern Altaids:Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen.Tectonophysics,499(1-4):118-131
Gao J,Wang XS,Klemd R,Jiang T,Qian Q,Mu LX and Ma YZ.2015.Record of assembly and breakup of Rodinia in the southwestern Altaids:Evidence from Neoproterozoic magmatism in the Chinese Western Tianshan Orogen.Journal of Asian Earth Sciences,113:173-193
Gao J,Zhu MT,Wang XS,Hong T,Li GM,Li JL,Xiao WJ,Qin KZ,Zeng QD,Shen P,Xu XW,Zhang ZC,Zhou JB,Lai Y,Zhang XH,Sun JG,Wan B and Wang B.2019.Large-scale porphyry-type mineralization in the Central Asian metallogenic domain:Tectonic background,fluid feature and metallogenic deep dynamic mechanism.Acta Geologica Sinica,93(1):24-71(in Chinese with English abstract)
Ge RF,Zhu WB,Wu HL,Zheng BH,Zhu XQ and He JW.2012.The Paleozoic northern margin of the Tarim Craton:Passive or active?Lithos,142-143:1-15
Ge RF,Zhu WB,Wu HL,He JW and Zheng BH.2013a.Zircon U-Pb ages and Lu-Hf isotopes of Paleoproterozoic metasedimentary rocks in the Korla Complex,NW China:Implications for metamorphic zircon formation and geological evolution of the Tarim Craton.Precambrian Research,231:1-18
Ge RF,Zhu WB,Wu HL,Zheng BH and He JW.2013b.Timing and mechanisms of multiple episodes of migmatization in the Korla Complex,northern Tarim Craton,NW China:Constraints from zircon U-Pb-Lu-Hf isotopes and implications for crustal growth.Precambrian Research,231:136-156
Ge RF,Zhu WB,Wilde SA,Wu HL,He JW and Zheng BH.2014a.Archean magmatism and crustal evolution in the northern Tarim Craton:Insights from zircon U-Pb-Hf-O isotopes and geochemistry of~2.7Ga orthogneiss and amphibolite in the Korla Complex.Precambrian Research,252:145-165
Ge RF,Zhu WB,Wilde SA,He JW,Cui X,Wang X and Zheng BH.2014b.Neoproterozoic to Paleozoic long-lived accretionary orogeny in the northern Tarim Craton.Tectonics,33(3):302-329
Ge RF,Zhu WB and Wilde SA.2016.Mid-Neoproterozoic(ca.830~800Ma)metamorphic P-T paths link Tarim to the circum-Rodinia subduction-accretion system.Tectonics,35(6):1465-1488
Gerdes A and Zeh A.2009.Zircon formation versus zircon alteration:New insights from combined U-Pb and Lu-Hf in-situ LA-ICP-MSanalyses,and consequences for the interpretation of Archean zircon from the Central Zone of the Limpopo Belt.Chemical Geology,261(3-4):230-243
Griffin WL,Belousova EA,Shee SR,Pearson NJ and O’Reilly SY.2004.Archean crustal evolution in the northern Yilgarn Craton:U-Pb and Hf-isotope evidence from detrital zircons.Precambrian Research,131(3-4):231-282
Han YG,Zhao GC,Sun M,Eizenh9fer PR,Hou WZ,Zhang XR,Liu DX,Wang B and Zhang GW.2015.Paleozoic accretionary orogenesis in the Paleo-Asian Ocean:Insights from detrital zircons from Silurian to Carboniferous strata at the northwestern margin of the Tarim Craton.Tectonics,34(2):334-351
Harper GD.2003.Fe-Ti basalts and propagating-rift tectonics in the Josephine ophiolite.Geological Society of America Bulletin,115(7):771-787
Hawkesworth C,Cawood P,Kemp T,Storey C and Dhuime B.2009.Amatter of preservation.Science,323(5910):49-50
Hawkesworth CJ,Gallagher K,Hergt JM and Mc Dermott F.1993.Mantle and slab contributions in arc magmas.Annual Review of Earth and Planetary Sciences,21(1):175-204
He ZY,Zhang ZM,Zong KQ,Wang W and Santosh M.2012.Neoproterozoic granulites from the northeastern margin of the Tarim Craton:Petrology,zircon U-Pb ages and implications for the Rodinia assembly.Precambrian Research,212-213:21-33
He ZY,Klemd R,Zhang ZM,Zong KQ,Sun LX,Tian ZL and Huang BT.2015.Mesoproterozoic continental arc magmatism and crustal growth in the eastern Central Tianshan Arc Terrane of the southern Central Asian Orogenic Belt:Geochronological and geochemical evidence.Lithos,236-237:74-89
He ZY,Wang B,Zhong LL and Zhu XY.2018a.Crustal evolution of the Central Tianshan Block:Insights from zircon U-Pb isotopic and structural data from meta-sedimentary and meta-igneous rocks along the Wulasitai-Wulanmoren shear zone.Precambrian Research,314:111-128
He ZY,Klemd R,Yan LL and Zhang ZM.2018b.The origin and crustal evolution of microcontinents in the Beishan orogen of the southern Central Asian Orogenic Belt.Earth-Science Reviews,185:1-14
Hu AQ,Zhang GX,Zhang QF and Chen YB.1998.Constraints on the age of basement and crustal growth in Tianshan Orogen by Nd isotopic composition.Science in China(Series D),41(6):648-657
Hu AQ,Wei GJ,Jahn BM,Zhang JB,Deng WF and Chen LL.2010.Formation of the 0.9Ga Neoproterozoic granitoids in the Tianshan Orogen,NW China:Constraints from the SHRIMP zircon age determination and its tectonic significance.Geochimica,39(3):197-212(in Chinese with English abstract)
Huang H,Zhang ZC,Santosh M,Zhang DY,Zhao ZD and Liu JL.2013.Early Paleozoic tectonic evolution of the South Tianshan collisional belt:Evidence from geochemistry and zircon U-Pb geochronology of the Tie’reke monzonite pluton,Northwest China.The Journal of Geology,121(4):401-424
Huang ZY,Long XP,Kr9ner A,Yuan C,Wang YJ,Chen B and Zhang YY.2015.Neoproterozoic granitic gneisses in the Chinese Central Tianshan Block:Implications for tectonic affinity and Precambrian crustal evolution.Precambrian Research,269:73-89
Huang ZY,Long XP,Yuan C,Sun M,Wang YJ,Zhang YY and Chen B.2016.Detrital zircons from Neoproterozoic sedimentary rocks in the Yili Block:Constraints on the affinity of microcontinents in the southern Central Asian Orogenic Belt.Gondwana Research,37:39-52
Huang ZY,Long XP,Wang XC,Zhang YY,Du L,Yuan C and Xiao WJ.2017.Precambrian evolution of the Chinese Central Tianshan Block:Constraints on its tectonic affinity to the Tarim Craton and responses to supercontinental cycles.Precambrian Research,295:24-37
Irvine TN and Baragar WRA.1971.A guide to the chemical classification of the common volcanic rocks.Canadian Journal of Earth Sciences,8(5):523-548
Jiang T,Gao J,Klemd R,Qian Q,Zhang X,Xiong XM,Wang XS,Tan Z and Chen BX.2014.Paleozoic ophiolitic mélanges from the South Tianshan Orogen,NW China:Geological,geochemical and geochronological implications for the geodynamic setting.Tectonophysics,612-613:106-127
Johannes W and Gupta LN.1982.Origin and evolution of a migmatite.Contributions to Mineralogy and Petrology,79(2):114-123
Johannes W,Holtz F and M9ller P.1995.REE distribution in some layered migmatites:Constraints on their petrogenesis.Lithos,35(3-4):139-152
Johannes W,Ehlers C,Kriegsman LM and Mengel K.2003.The link between migmatites and S-type granites in the Turku area,southern Finland.Lithos,68(3-4):69-90
Kelley KA and Cottrell E.2009.Water and the oxidation state of subduction zone magmas.Science,325(5940):605-607
Kriegsman LM.2001.Partial melting,partial melt extraction and partial back reaction in anatectic migmatites.Lithos,56(1):75-96
Kr9ner A,Windley BF,Badarch G,Tomurtogoo O,Hegner E,Jahn BM,Gruschka S,Khain EV,Demoux A and Wingate MTD.2007.Accretionary growth and crust formation in the Central Asian Orogenic Belt and comparison with the Arabian-Nubian shield.Geological Society of America Memoirs,200:181-209
Kr9ner A,Alexeiev DV,Rojas-Agramonte Y,Hegner E,Wong J,Xia X,Belousova E,Mikolaichuk AV,Seltmann R,Liu DY and Kiselev VV.2013.Mesoproterozoic(Grenville-age)terranes in the Kyrgyz North Tianshan:Zircon ages and Nd-Hf isotopic constraints on the origin and evolution of basement blocks in the southern Central Asian Orogen.Gondwana Research,23(1):272-295
Kr9ner A,Alexeiev DV,Kovach VP,Rojas-Agramonte Y,Tretyakov AA,Mikolaichuk AV,Xie H and Sobel ER.2017a.Zircon ages,geochemistry and Nd isotopic systematics for the Palaeoproterozoic 2.3~1.8Ga Kuilyu Complex,East Kyrgyzstan:The oldest continental basement fragment in the Tianshan orogenic belt.Journal of Asian Earth Sciences,135:122-135
Kr9ner A,Kovach V,Alexeiev D,Wang KL,Wong J,Degtyarev K and Kozakov I.2017b.No excessive crustal growth in the Central Asian Orogenic Belt:Further evidence from field relationships and isotopic data.Gondwana Research,50:135-166
Kruckenberg SC,Vanderhaeghe O,FerréEC,Teyssier C and Whitney DL.2011.Flow of partially molten crust and the internal dynamics of a migmatite dome,Naxos,Greece.Tectonics,30(3):TC3001
Li Q and Zhang LF.2004.The P-T path and geological significance of low-pressure granulite-facies metamorphism in Muzhaerte,Southwest Tianshan.Acta Petrologica Sinica,20(3):583-594(in Chinese with English abstract)
Li XH,Liu Y,Li QL,Guo CH and Chamberlain KR.2009.Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization.Geochemistry,Geophysics,Geosystems,10(4):Q04010
Long LL,Gao J,Klemd R,Beier C,Qian Q,Zhang X,Wang JB and Jiang T.2011a.Geochemical and geochronological studies of granitoid rocks from the Western Tianshan Orogen:Implications for continental growth in the southwestern Central Asian Orogenic Belt.Lithos,126(3-4):321-340
Long XP,Yuan C,Sun M,Kr9ner A,Zhao GC,Wilde S and Hu AQ.2011b.Reworking of the Tarim Craton by underplating of mantle plume-derived magmas:Evidence from Neoproterozoic granitoids in the Kuluketage area,NW China.Precambrian Research,187(1-2):1-14
Long XP and Huang ZY.2017.Tectonic affinities of microcontinents in the Central Asian Orogenic Belt:A case study of the Chinese Tianshan orogenic belt.Bulletin of Mineralogy,Petrology and Geochemistry,36(5):771-785(in Chinese with English abstract)
Ludwig KR.2003.User’s manual for Isoplot 3.00:A geochronological toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication,4:1-70
Luo FZ.1989.On Precambrian in mid-Tianshan uplift(metamorphic)zone.Xinjiang Geology,7(4):24-33(in Chinese with English abstract)
Ma XX,Shu LS,Santosh M and Li JY.2012a.Detrital zircon U-Pb geochronology and Hf isotope data from Central Tianshan suggesting a link with the Tarim Block:Implications on Proterozoic supercontinent history.Precambrian Research,206-207:1-16
Ma XX,Shu LS,Jahn BM,Zhu WB and Faure M.2012b.Precambrian tectonic evolution of Central Tianshan,NW China:Constraints from U-Pb dating and in situ Hf isotopic analysis of detrital zircons.Precambrian Research,222-223:450-473
Ma XX,Shu LS,Santosh M and Li JY.2013a.Paleoproterozoic collisional orogeny in Central Tianshan:Assembling the Tarim Block within the Columbia supercontinent.Precambrian Research,228:1-19
Ma XX,Shu LS,Santosh M and Li JY.2013b.Petrogenesis and tectonic significance of an Early Palaeozoic mafic-intermediate suite of rocks from the Central Tianshan,Northwest China.International Geology Review,55(5):548-573
Martin H,Smithies RH,Rapp R,Moyen JF and Champion D.2005.An overview of adakite,tonalite-trondhjemite-granodiorite(TTG),and sanukitoid:Relationships and some implications for crustal evolution.Lithos,79(1-2):1-24
Martin LAJ,Duchêne S,Deloule E and Vanderhaeghe O.2008.Mobility of trace elements and oxygen in zircon during metamorphism:Consequences for geochemical tracing.Earth and Planetary Science Letters,267(1-2):161-174
Mehnert KR.1968.Migmatites and the Origin of Granitic Rocks.Amsterdam:Elsevier
Meschede M.1986.A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Ydiagram.Chemical Geology,56(3-4):207-218
Moyen JF and Martin H.2012.Forty years of TTG research.Lithos,148:312-336
Pearce JA.2008.Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust.Lithos,100(1-4):14-48
Peng P,Zhai MG,Zhang HF,Zhao TP and Ni ZY.2004.Geochemistry and geological significance of the 1.8Ga mafic dyke swarms in the North China Craton:An example from the juncture of Shanxi,Hebei and Inner Mongolia.Acta Petrologica Sinica,20(3):439-456(in Chinese with English abstract)
Prouteau G,Scaillet B,Pichavant M and Maury R.2001.Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust.Nature,410(6825):197-200
Qian Q,Gao J,Klemd R,He GQ,Song B,Liu DY and Xu RH.2009.Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen:Constraints from SHRIMP zircon U-Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate,NW China.International Journal of Earth Sciences,98(3):551-569
Rojas-Agramonte Y,Herwartz D,García-Casco A,Kr9ner A,Alexeiev DV,Klemd R,Buhre S and Barth M.2013.Early Palaeozoic deep subduction of continental crust in the Kyrgyz North Tianshan:Evidence from Lu-Hf garnet geochronology and petrology of mafic dikes.Contributions to Mineralogy and Petrology,166(2):525-543
Rollinson HR.2014.Using Geochemical Data:Evaluation,Presentation,Interpretation.London:Routledge,1-351
Sawyer EW and Robin PYF.1986.The subsolidus segregation of layerparallel quartz-feldspar veins in greenschist to upper amphibolite facies metasediments.Journal of Metamorphic Geology,4(3):237-260
Sawyer EW.1996.Melt segregation and magma flow in migmatites:Implications for the generation of granite magmas.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,87(1-2):85-94
Sawyer EW.2008.Atlas of Migmatites.The Canadian Mineralogist,Special Publication 9.Ottawa:NRC Research Press,1-371
Sclar CB.1965.Layered mylonites and the processes of metamorphic differentiation.GSA Bulletin,76(5):611-612
Sederholm JJ.1907.Om granit och gneis deras uppkomst:Upptrdande och utbredning inom urberget i Fennos-kandia.Bulletin de la Commission geologique de Finlande,23
S9derlund U,Patchett PJ,Vervoort JD and Isachsen CE.2004.The176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions.Earth and Planetary Science Letters,219(3-4):311-324
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basin.Geological Society,London,Special Publications,42(1):313-345
Thy P,Lesher CE and Tegner C.2009.The Skaergaard liquid line of descent revisited.Contributions to Mineralogy and Petrology,157(6):735-747
Turner FJ.1941.The development of pseudo-stratification by metamorphic differentiation in the schists of Otago,New Zealand.American Journal of Science,239(1):1-16
Vervoort JD and Blichert-Toft J.1999.Evolution of the depleted mantle:Hf isotope evidence from juvenile rocks through time.Geochimica et Cosmochimica Acta,63(3-4):533-556
Wan B,Windley BF,Xiao WJ,Feng JY and Zhang JE.2015.Paleoproterozoic high-pressure metamorphism in the northern North China Craton and implications for the Nuna supercontinent.Nature Communications,6:8344
Wang B,Faure M,Cluzel D,Shu LS,Charvet J,Meffre S and Ma Q.2006.Late Paleozoic tectonic evolution of the northern West Chinese Tianshan belt.Geodinamica Acta,19(3-4):237-247
Wang B,Shu LS,Faure M,Cluzel D and Charvet J.2007.Paleozoic tectonism and magmatism of Kekesu-Qiongkushitai section in southwestern Chinese Tianshan and their constraints on the age of the orogeny.Acta Petrologica Sinica,23(6):1354-1368(in Chinese with English abstract)
Wang B,Shu LS,Faure M,Jahn BM,Cluzel D,Charvet J,Chung SLand Meffre S.2011.Paleozoic tectonics of the southern Chinese Tianshan:Insights from structural,chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China).Tectonophysics,497(1-4):85-104
Wang B,Jahn BM,Shu LS,Li KS,Chung SL and Liu DY.2012.Middle-Late Ordovician arc-type plutonism in the NW Chinese Tianshan:Implication for the accretion of the Kazakhstan continent in Central Asia.Journal of Asian Earth Sciences,49:40-53
Wang B,Liu HS,Shu LS,Jahn BM,Chung SL,Zhai YZ and Liu DY.2014a.Early Neoproterozoic crustal evolution in northern Yili Block:Insights from migmatite,orthogneiss and leucogranite of the Wenquan metamorphic complex in the NW Chinese Tianshan.Precambrian Research,242:58-81
Wang B,Zhai YZ,Kapp P,de Jong K,Zhong LL,Liu HS,Ma YZ,Gong HJ and Geng HY.2018c.Accretionary tectonics of back-arc oceanic basins in the South Tianshan:Insights from structural,geochronological,and geochemical studies of the Wuwamen ophiolite mélange.Geological Society of America Bulletin,130(1-2):284-306
Wang XS,Gao J,Klemd R,Jiang T,Li JL,Zhang X,Tan Z,Li L and Zhu ZX.2014b.Geochemistry and geochronology of the Precambrian high-grade metamorphic complex in the southern Central Tianshan ophiolitic mélange,NW China.Precambrian Research,254:129-148
Wang XS,Gao J,Klemd R,Jiang T,Zhai QG,Xiao XC and Liang XQ.2015.Early Neoproterozoic multiple arc-back-arc system formation during subduction-accretion processes between the Yangtze and Cathaysia blocks:New constraints from the supra-subduction zone NE Jiangxi ophiolite(South China).Lithos,236-237:90-105
Wang XS,Gao J,Klemd R,Jiang T,Li JL,Zhang X and Xue SC.2017.The Central Tianshan Block:A microcontinent with a Neoarchean-Paleoproterozoic basement in the southwestern Central Asian Orogenic Belt.Precambrian Research,295:130-150
Wang XS,Klemd R,Gao J,Jiang T,Li JL and Xue SC.2018a.Final assembly of the southwestern Central Asian Orogenic Belt as constrained by the evolution of the South Tianshan Orogen:Links with Gondwana and Pangea.Journal of Geophysical Research:Solid Earth,123(9):7361-7388
Wang XS,Zhang X,Gao J,Li JL,Jiang T and Xue SC.2018b.A slab break-off model for the submarine volcanic-hosted iron mineralization in the Chinese Western Tianshan:Insights from Paleozoic subduction-related to post-collisional magmatism.Ore Geology Reviews,92:144-160
Wiedenbeck M,AlléP,Corfu F,Griffin WL,Meier M,Oberli F,von Quadt A,Roddick JC and Spiegel W.1995.Three natural zircon standards for U-Th-Pb,Lu-Hf,trace element and REE analyses.Geostandards Newsletter,19(1):1-23
Wilhem C,Windley BF and Stampfli GM.2012.The Altaids of Central Asia:A tectonic and evolutionary innovative review.Earth-Science Reviews,113(3-4):303-341
Winchester JA and Floyd PA.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325-343
Windley BF,Alexeiev D,Xiao WJ,Kr9ner A and Badarch G.2007.Tectonic models for accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164(1):31-47
Wood DA.1980.The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province.Earth and Planetary Science Letters,50(1):11-30
Wu FY,Yang YH,Xie LW,Yang JH and Xu P.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1-2):105-126
Xia B,Zhang LF and Bader T.2014.Zircon U-Pb ages and Hf isotopic analyses of migmatite from the‘paired metamorphic belt’in Chinese SW Tianshan:Constraints on partial melting associated with orogeny.Lithos,192-195:158-179
Xiao WJ,Windley BF,Yuan C,Sun M,Han CM,Lin SF,Chen HL,Yan QR,Liu DY,Qin KZ,Li JL and Sun S.2009.Paleozoic multiple subduction-accretion processes of the southern Altaids.American Journal of Science,309(3):221-270
Xiao WJ,Windley BF,Allen MB and Han CM.2013.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage.Gondwana Research,23(4):1316-1341
Xiao WJ,Windley BF,Sun S,Li JL,Huang BC,Han CM,Yuan C,Sun M and Chen HL.2015.A tale of amalgamation of three PermoTriassic collage systems in Central Asia:Oroclines,sutures,and terminal accretion.Annual Review of Earth and Planetary Sciences,43(1):477-507
Xu YG,Mei HJ,Xu JF,Huang XL,Wang YJ and Chung SL.2003.Origin of two differentiation trends in the Emeishan flood basalts.Chinese Science Bulletin,48(4):390-394
Yang XS,Jin ZM and Ma J.2005.Anatexis in Himalayan crust:Evidence from geochemical and chronological investigations of Higher Himalayan Crystallines.Science in China(Series D),48(9):1347-1356
Zhang CL,Li XH,Li ZX,Lu SN,Ye HM and Li HM.2007.Neoproterozoic ultramafic-mafic-carbonatite complex and granitoids in Quruqtagh of northeastern Tarim Block,western China:Geochronology,geochemistry and tectonic implications.Precambrian Research,152(3-4):149-169
Zhang CL,Li HK and Wang HY.2012.A review on Precambrian tectonic evolution of Tarim Block:Possibility of interaction between Neoproterozoic plate subduction and mantle plume.Geological Review,58(5):923-936(in Chinese with English abstract)
Zhang J,Zhang CL,Li HK,Ye XT,Geng JZ and Zhou HY.2014.Revisit to time and tectonic environment of the Aksu blueschist terrane in northern Tarim,NW China:New evidence from zircon U-Pb age and Hf isotope.Acta Petrologica Sinica,30(11):3357-3365(in Chinese with English abstract)
Zhang X,Klemd R,Gao J,Dong LH,Wang XS,Haase K,Jiang T and Qian Q.2015.Metallogenesis of the Zhibo and Chagangnuoer volcanic iron oxide deposits in the Awulale Iron Metallogenic Belt,Western Tianshan orogen,China.Journal of Asian Earth Sciences,113:151-172
Zhao GC,Cawood PA,Wilde SA and Sun M.2002.Review of global2.1~1.8Ga orogens:Implications for a pre-Rodinia supercontinent.Earth-Science Reviews,59(1-4):125-162
Zhong LL,Wang B,Shu LS,Liu HS,Mu LX,Ma YZ and Zhai YZ.2015.Structural overprints of Early Paleozoic arc-related intrusive rocks in the Chinese Central Tianshan:Implications for Paleozoic accretionary tectonics in SW Central Asian Orogenic Belts.Journal of Asian Earth Sciences,113:194-217
Zhu YF,Zhou J,Song B,Zhang LF and Guo X.2006.Age of the“Dahalajunshan”Formation in Xinjiang and its disintegration.Geology in China,33(3):487-497(in Chinese with English abstract)
程裕淇．1987．有关混合岩和混合岩化作用的一些问题---对半个世纪以来某些基本认识的回顾．中国地质科学院院报，16:5-19
高俊，钱青，龙灵利，张喜，李继磊，苏文．2009．西天山的增生造山过程．地质通报，28(12):1804-1816
高俊，朱明田，王信水，洪涛，李光明，李继磊，肖文交，秦克章，曾庆栋，申萍，徐兴旺，张招崇，周建波，赖勇，张晓晖，孙景贵，万博，王博．2019．中亚成矿域斑岩大规模成矿特征:大地构造背景、流体作用与成矿深部动力学机制．地质学报，93(1):24-71
胡霭琴，韦刚健，江博明，张积斌，邓文峰，陈林丽．2010．天山0.9Ga新元古代花岗岩SHRIMP锆石U-Pb年龄及其构造意义．地球化学，39(3):197-212
李强，张立飞．2004．新疆西南天山木扎尔特一带低压麻粒岩相变质作用P-T轨迹及其地质意义．岩石学报，20(3):583-594
龙晓平，黄宗莹．2017．中亚造山带内微陆块的起源---以中国天山造山带研究为例．矿物岩石地球化学通报，36(5):771-785
罗发祚．1989．对中天山隆起(变质)带前寒武系的探讨．新疆地质，7(4):24-33
彭澎，翟明国，张华锋，赵太平，倪志耀．2004．华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例．岩石学报，20(3):439-456
王博，舒良树，Faure M,Cluzel D,Charvet J.2007．科克苏-穹库什太古生代构造-岩浆作用及其对西南天山造山时代的约束．岩石学报，23(6):1354-1368
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
张传林，李怀坤，王洪燕．2012．塔里木地块前寒武纪地质研究进展评述．地质论评，58(5):923-936
张健，张传林，李怀坤，叶现韬，耿建珍，周红英．2014．再论塔里木北缘阿克苏蓝片岩的时代和成因环境:来自锆石U-Pb年龄、Hf同位素的新证据．岩石学报，30(11):3357-3365
朱永峰，周晶，宋彪，张立飞，郭璇．2006．新疆“大哈拉军山组”火山岩的形成时代问题及其解体方案．中国地质，33(3):487-497
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |