华北克拉通东部及苏鲁造山带的地壳生长:来自现代河流碎屑锆石的U-Pb定年和Hf同位素证据
摘要
来自年轻沉积物或现代河流的碎屑锆石是研究大陆地壳生长演化的理想载体.为揭示华北克拉通东部和苏鲁造山带大陆地壳的生长演化,采集了中国东部大清河、潮白河、辽河、大沽河和胶莱河的5个地方的河沙样品,并对分选出来的碎屑锆石进行了LA-ICP-MS和MC-LA-ICP-MS U-Pb定年和Hf同位素微区原位分析,获得了396个锆石U-Pb谐和年龄及其对应的Hf同位素组成.2.4~2.5 Ga和1.8~1.9 Ga两个年龄特征峰指示大清河、潮白河和辽河的碎屑锆石来源于华北克拉通东部.辽河一部分100~500 Ma的锆石具有正的εHf(t)值和年轻的Hf模式年龄,显示出显生宙的地壳生长.苏鲁造山带大沽河和胶莱河的碎屑锆石U-Pb年龄分布相对比较复杂,但锆石U-Pb年龄和Hf同位素特征表明其为华北克拉通和扬子克拉通的混合来源.来自大清河、潮白河和辽河的锆石U-Pb年龄和Hf同位素证据,表明华北克拉通东部地壳生长的主要时期为2.4~3.0 Ga,并在2.6~2.7 Ga时处于生长的最高峰,次一级的生长期为1.3~2.3 Ga,而在其他阶段几乎没有地壳的生长或者不明显.华北克拉通东部现存大陆地壳的80%来源于太古代和古元古代的生长,而自古元古代开始大陆地壳的演化就以古老地壳的重熔再改造为主.此外,大沽河碎屑锆石的Hf同位素组成揭示出苏鲁造山带在古生代(300~500 Ma)存在明显的地壳生长.
Detrial zircon from clastic sediment or sands of modern rivers is an ideal sample for studying the growth and evolution of the continental crust.In order to reveal the crustal growth of eastern North China craton and Sulu orogen,396 concordant detrital zircons in three sand samples from the Daqing River,Chaobai River,Liao River,Dagu River and Jiaolai River in eastern North China were measured for U-Pb age and Hf isotopic compositions by excimer laser-ablation ICP-MS and MC-ICP-MS,respectively.The Daqing River,Chaobai River and Liao River are characterized by two age peaks of 2.4-2.5 Ga and 1.8-1.9 Ga,which indicate contributions from the eastern North China craton.Some 100-500 Ma zircons from the Liao River with positive εHf(t) values and young Hf model ages,suggesting Phanerozoic crustal growth.In contrast,U-Pb ages of the Dagu River and Jiaolai River,which run through the Sulu orogen,are more complicated and characterized by age groups of 2.4-2.5 Ga,1.8-1.9 Ga and 700-800 Ma,implying a mixed provenance of eastern North China craton and Yangtze craton.The Lu-Hf isotope compositions of the Daqing River,Chaobai River and Liao River demonstrate the dominant growth at 2.4-3.0 Ga,with a peak at 2.6-2.7 Ga and minor growth during 1.3-2.3 Ga.However,there is insignificant crustal growth during other periods.In addition,80% of the existing crust in eastern North China craton was produced before Paleoproterozoic and reworking of preexisting continental crust became dominant since then.Meanwhile,a Paleozoic(300-500 Ma) crustal growth characterizes zircon Hf isotopes of the Dagu River of the Sulu orogen.
Detrial zircon from clastic sediment or sands of modern rivers is an ideal sample for studying the growth and evolution of the continental crust.In order to reveal the crustal growth of eastern North China craton and Sulu orogen,396 concordant detrital zircons in three sand samples from the Daqing River,Chaobai River,Liao River,Dagu River and Jiaolai River in eastern North China were measured for U-Pb age and Hf isotopic compositions by excimer laser-ablation ICP-MS and MC-ICP-MS,respectively.The Daqing River,Chaobai River and Liao River are characterized by two age peaks of 2.4-2.5 Ga and 1.8-1.9 Ga,which indicate contributions from the eastern North China craton.Some 100-500 Ma zircons from the Liao River with positive εHf(t) values and young Hf model ages,suggesting Phanerozoic crustal growth.In contrast,U-Pb ages of the Dagu River and Jiaolai River,which run through the Sulu orogen,are more complicated and characterized by age groups of 2.4-2.5 Ga,1.8-1.9 Ga and 700-800 Ma,implying a mixed provenance of eastern North China craton and Yangtze craton.The Lu-Hf isotope compositions of the Daqing River,Chaobai River and Liao River demonstrate the dominant growth at 2.4-3.0 Ga,with a peak at 2.6-2.7 Ga and minor growth during 1.3-2.3 Ga.However,there is insignificant crustal growth during other periods.In addition,80% of the existing crust in eastern North China craton was produced before Paleoproterozoic and reworking of preexisting continental crust became dominant since then.Meanwhile,a Paleozoic(300-500 Ma) crustal growth characterizes zircon Hf isotopes of the Dagu River of the Sulu orogen.
引文
Andersen,T.,2002.Correction of commonleadin U-Pb analysesthat do not report204Pb.Chemical Geology,192(1-2):59-79.doi:10.1016/s0009-2541(02)00195-x
Bichert-Toft,J.,Albarède,F.,1997.The Lu-Hf isotope geo-chemistry of chondrites and the evolution of the mantle-crust system.Earth and Planetary Science Letters,148(1-2):243-258.doi:10.1016/s0012-821x(97)00040-x
Campbell,I.H.,Allen,C.M.,2008.Formation of supercon-tinents linked to increases in at mospheric oxygen.Na-ture Geoscience,1(8):554-558.doi:10.1038/ngeo259
Cawood,P.A.,Nemchin,A.A.,Strachan,R.,et al.,2007.Sedimentary basin and detrital zircon record along EastLaurentia and Baltica during assembly and breakup ofRodinia.Journal ofthe Geological Society,164(2):257-275.doi:10.1144/0016-76492006-115
Chen,B.,Jahn,B.M.,Tian,W.,2009.Evolution of the So-lonker suture zone:constraints fromzircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compo-sitions of subduction-and collision-related magmas andforearc sediments.Journal of Asian Earth Sciences,34(3):245-257.doi:10.1016/j.jseaes.2008.05.007
Chen,B.,Jahn,B.M.,Wilde,S.,et al.,2000.Two contras-ting paleozoic magmatic belts in northern Inner Mongo-lia,China:petrogenesis and tectonic implications.Tec-tonophysics,328(1-2):157-182.doi:10.1016/s0040-1951(00)00182-7
Cheng,R.Y.,Wu,F.Y.,Ge,W.C.,et al.,2006.Emplace-ment age of the Raohe complex in eastern HeilongjiangProvince and the tectonic evolution of the eastern partof northeastern China.Acta Petrologica Sinica,22(2):353-376(in Chinese with English abstract).
Chu,N.C.,Taylor,R.N.,Chavagnac,V.,et al.,2002.Hfisotope ratio analysis using multi-collector inductivelycoupled plasma mass spectrometry:an evaluation ofisobaric interference corrections.Journal of AnalyticalAtomic Spectrometry,17(12):1567-1574.doi:10.1039/b206707b
Condie,K.C.,1998.Episodic continental growth and super-continents:a mantle avalanche connection Earth andPlanetary Science Letters,163(1-4):97-108.doi:10.1016/s0012-821x(98)00178-2
Condie,K.C.,2000.Episodic continental growth models:af-terthoughts and extensions.Tectonophysics,322(1-2):153-162.doi:10.1016/s0040-1951(00)00061-5
Condie,K.C.,Aster,R.C.,2010.Episodic zircon age spectraof orogenic granitoids:the supercontinent connectionand continental growth.Precambrian Research,180(3-4):227-236.doi:10.1016/j.precamres.2010.03.008
Condie,K.C.,Belousova,E.,Griffin,W.L.,et al.,2009.Gran-itoid events in space and time:constraints fromigneous anddetrital zircon age spectra.Gondwana Research,15(3-4):228-242.doi:10.1016/j.gr.2008.06.001
Condie,K.C.,Beyer,E.,Belousova,E.,et al.,2005.U-Pbisotopic ages and Hf isotopic composition of single zir-cons:the search for juvenile Precambrian continentalcrust.Precambrian Research,139(1-2):42-100.doi:10.1016/j.precamres.2005.04.006
Coogan,L.A.,Hinton,R.W.,2006.Do the trace element com-positions of detrital zircons require Hadean continentalcrust Geology,34(8):633-636.doi:10.1130/g22737
De Bieve,P.,Taylor,P.D.P.,1993.Table of the isotopiccomposition of elements.International Journal of MassSpectrometryIon and Process,123:149-166.doi:10.1016/0168-1176(93)87009-h
DePaolo,D.J.,Linn,A.M.,Schubert,G.,1991.The conti-nental crustal age distribution:methods of determiningmantle separation ages from Sm-Nd isotopic data andapplicatoin to the southwestern United States.Journalof Geophysical Research,96(B2):2071-2088.doi:10.1029/90jb02219
Fan,W.M.,Guo,F.,Wang,Y.J.,et al.,2003.Late Meso-zoic calc-alkaline volcanism of post-orogenic extensionin the northern Dahinggan Mountains,northeasternChina.Journal of Volcanology and Geothermal Re-search,121(1-2):115-135.doi:10.1016/s0377-0273(02)00415-8
Faure,M.,Lin,W.,Le Breton,N.,2001.Where is the NorthChina-South China block boundary in eastern China.Geology,29(2):119-122.doi:10.1130/0091-7613(2001)029<0119
Ferry,J.M.,Watson,E.B.,2007.Newthermodynamic mod-els and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers.Contributions to Mineralogyand Petrology,154(4):429-437.doi:10.1007/s00410-007-0201-0
Gao,S.,Rudnick,R.L.,Carlson,R.W.,et al.,2002.Re-Osevidence for replacement of ancient mantle lithospherebeneath the North China craton.Earth and PlanetaryScience Letters,198(3-4):307-322.doi:10.1016/s0012-821x(02)00489-2
Gao,S.,Rudnick,R.L.,Yuan,H.L.,et al.,2004.Recyclinglower continental crust in the North China craton.Na-ture,432(7019):892-897.doi:10.1038/nature03162
Gao,S.,Zhang,J.F.,Xu,W.L.,et al.,2009.Delaminationand destruction of the North China craton.Chinese Sci-ence Bulletin,54(19):3367-3378.doi:10.1007/s11434-009-0395-9
Ge,W.C.,Wu,F.Y.,Zhou,C.Y.,et al.,2005.Zircon U-Pbages and its significance of the Mesozoic granites in theWulanhaote region,Central Da Hinggan Mountain.ActaPetrologica Sinica,21(3):749-762(in Chinese withEnglish abstract).
Gilder,S.A.,Leloup,P.H.,Courtillot,V.,et al.,1999.Tectonic evolution of the Tancheng-Lujiang(Tan-Lu)fault via Middle Triassic to Early Cenozoic paleomag-netic data.Journal of Geophysical Research-SolidEarth,104(B7):15365-15390.doi:10.1029/1999jb900123
Goldschmidt,V.M.,1933.Grundlagen der quantitativen geo-chemie.Fortschritte der Mineralogic KirstlographiePetrographie,17:112.
Griffin,W.L.,Belousova,E.A.,Shee,S.R.,et al.,2004.Archean crustal evolution in the northern Yilgam cra-ton:U-Pb and Hf-isotope evidence from detrital zir-cons.Precambrian Research,131(3-4):231-282.doi:10.1016/j.precamres.2003.12.011
Hacker,B.R.,Wallis,S.R.,Mc Williams,M.O.,et al.,2009.40Ar/39Ar constraints on the tectonic history andarchitecture of the ultrahigh-pressure Sulu orogen.Journal of Metamorphic Geology,27(9):827-844.doi:10.1111/j.1525-1314.2009.00840.x
Hanchar,J.M.,Hoskin,P.W.O.,2003.Zircon:reviews inmineralogy and geochemistry.Mineralogical Society ofAmerica,53:500.
Hawkesworth,C.J.,Dhuime,B.,Pietranik,A.B.,et al.2010.The generation and evolution of the continentalcrust.Journal ofthe Geological Society,167(2):229-248.doi:10.1144/0016-76492009-072
Hawkesworth,C.J.,Kemp,A.I.S.,2006a.Evolution of thecontinental crust.Nature,443(7113):811-817.doi:10.1038/nature05191
Hawkesworth,C.J.,Kemp,A.I.S.,2006b.Using hafniumand oxygenisotopes in zircons to unravel the record ofcrustal evolution.Chemical Geology,226(3-4):144-162.doi:10.1016/j.chemgeo.2005.09.018
Hu,Z.C.,Gao,S.,2008.Upper crustal abundances of trace ele-ments:a revision and update.Chemical Geology,253(3-4):205-221.doi:10.1016/j.chemgeo.2008.05.010
Iizuka,T.,Hirata,T.,2005.Improvements of precision andaccuracy in in situ Hf isotope microanalysis of zirconusing the laser ablation-MC-ICPMS technique.Chemi-cal Geology,220(1-2):121-137.doi:10.1016/j.chemgeo.2005.03.010
Iizuka,T.,Hirata,T.,Komiya,T.,et al.,2005.U-Pb andLu-Hf isotope systematics of zircons from the Missis-sippi River sand:implications for reworking and growthof continental crust.Geology,33(6):485-488.doi:10.1130/g21427.1
Jackson,S.E.,Pearson,N.J.,Griffin,W.L.,et al.,2004.The application of laser ablation-inductively coupledplasma-mass spectrometry to in situ U-Pb zircon geo-chronology.Chemical Geology,211(1-2):47-69.doi:10.1016/j.chemgeo.2004.06.017
Jahn,B.M.,Capdevila,R.,Liu,D.Y.,et al.,2004.Sourcesof Phanerozoic granitoids in the transect Bayanhongor-Ulaan Baatar,Mongolia:geochemical and Nd isotopicevidence,and implications for Phanerozoic crustalgrowth.Journal of Asian Earth Sciences,23(5):629-653.doi:10.1016/s1367-9120(03)00125-1
Jahn,B.M.,Wu,F.Y.,Capdevila,R.,et al.,2001.Highlyevolved juvenile granites with tetrad REE patterns:theWoduhe and Baerzhe granites from the Great Xing anMountains in NE China.Lithos,59(4):171-198.doi:10.1016/s0024-4937(01)00066-4
Jahn,B.M.,Wu,F.Y.,Chen,B.,2000a.Granitoids of theCentral Asian orogenic belt and continental growth inthe Phanerozoic.Transactions of the Royal Society ofEdinburgh:Earth and Environmental Sciences,350:181-193.doi:10.1130/0-8137
Jahn,B.M.,Wu,F.Y.,Hong,D.W.,2000b.Importantcrustal growth in the Phanerozoic:isotopic evidence ofgranitoids from East-Central Asia.Proceedings of theIndian Academy of Sciences-Earth and Planetary Sci-ences,109(1):5-20.doi:10.1007/bf02719146
Jian,P.,Liu,D.Y.,Kroner,A.,et al.,2008.Time scale ofan early to Mid-Paleozoic orogenic cycle of the long-lived Central Asian orogenic belt,Inner Mongolia ofChina:implications for continental growth.Lithos,101(3-4):233-259.doi:10.1016/j.lithos.2007.07.005
Kemp,A.I.S.,Hawkesworth,C.J.,Paterson,B.A.,et al.,2006.Episodic growth of the Gondwana supercontinentfrom hafnium and oxygen isotopes in zircon.Nature,439(7076):580-583.doi:10.1038/nature04505
Kusky,T.M.,Santosh,M.,2009.The Columbia connectionin North China.Geological Society of London:SpecialPublications,323:49-71.doi:10.1144/sp323.3
Li,S.Z.,Kusky,T.M.,Liu,X.C.,et al.,2009.Two-stage col-lision-related extrusion of the western Dabie HP-UHPmetamorphic terranes,Central China:evidence fromquartzc-axis fabrics and structures.Gondwana Research,16(2):294-309.doi:10.1016/j.gr.2009.03.003
Li,X.H.,Li,Z.X.,Ge,W.C.,et al.,2003.Neoproterozoicgranitoids in South China:crustal melting above a mantleplume at ca.825Ma.Precambrian Research,122(1-4):45-83.doi:10.1016/s0301-9268(02)00207-3
Li,X.H.,Li,Z.X.,Zhou,H.W.,et al.,2002.U-Pb zircongeochronology,geochemistry and Nd isotopic study ofNeoproterozoic bimodal volcanic rocks in the KangdianRift of South China:implications for the initial riftingof Rodinia.Precambrian Research,113(1-2):135-154.doi:10.1016/s0301-9268(01)00207-8
Li,Z.X.,1994.Collision between the North and South Chinablocks:a crustal-detachment model for suturinginthe regioneast of the Tanlu fault.Geology,22(8):739-742.doi:10.1130/0091-7613(1995)023<0574:cbtnas>2.3.CO
Liu,D.Y.,Nut man,A.P.,Compston,W.,et al.,1992.Remnants of≥3800Ma crust inthe Chinese part of theSino-Korean craton.Geology,20(4):339-342.doi:10.1130/0091-7613(1992)020<0339:romcit>2.3.CO
Liu,W.,Siebel,W.,Li,X.J.,et al.,2005.Petrogenesis of theLinxi granitoids,northern Inner Mongolia of China:con-straints on basaltic underplating.Chemical Geology,219(1-4):5-35.doi:10.1016/j.chemgeo.2005.01.013
Liu,X.M.,Gao,S.,Di wu,C.R.,et al.,2008.Precambriancrustal growth of Yangtze craton as revealed by detritalzircon studies.American Journal of Science,308(4):421-468.doi:10.2475/04.2008.02
Ludwig,K.R.,2003.ISOPLOT3:a geochronological toolkitfor Microsoft Excel.Berkeley Geochronology CentreSpecial Publication,Berkeley,California,70.
McLennan,S.M.,2001.Relationships between the trace ele-ment composition of sedimentary rocks and upper conti-nental crust.Geochemistry Geophysics Geosystems,2(4):1021-1044.doi:10.1029/2000gc000109
Meng,F.X.,Gao,S.,Yuan,H.L.,et al.,2010.Permian-tri-assic(260-220Ma)crustal growth of eastern centralAsian orogenic belt as revealed by detrital zircon stud-ies.American Journal of Science,310(5):364-404.doi:10.2475/05.2010.02
Meng,Q.R.,Zhang,G.W.,2000.Geologic framework andtectonic evolution of the Qinling orogen,central China.Tectonophysics,323(3-4):183-196.doi:10.1016/s0040-1951(00)00106-2
Miao,L.C.,Fan,W.M.,Liu,D.Y.,et al.,2008.Geochro-nology and geochemistry of the Hegenshan ophioliticcomplex:implications for late-stage tectonic evolutionof the Inner Mongolia-Daxinganling orogenic belt,Chi-na.Journal of Asian Earth Sciences,32(5-6):348-370.doi:10.1016/j.jseaes.2007.11.005
Oh,C.W.,Kusky,T.,2007.The Late Permian to TriassicHongseong-odesan collision belt in South Korea,anditstectonic correlation with China and Japan.InternationalGeology Review,49(7):636-657.doi:10.2747/0020-6814.49.7.636
Okay,A.I.,Seng r,A.M.C.,1992.Evidence for intraconti-nental thrust-related exhumation of the ultra-high-pres-sure rocks in China.Geology,20(5):411-414.doi:10.1130/0091-7613(1992)020<0411:efitre>2.3.CO
Pietranik,A.B.,Hawkesworth,C.J.,Storey,C.D.,et al.,2008.Episodic,mafic crust formation from4.5to2.8Ga:new evidence from detrital zircons,Slave craton,Canada.Geology,36(11):875-878.doi:10.1130/g24861a.1
Rudnick,R.L.,Gao,S.,2003.Composition of the continentalcrust:the crust:treatise on geochemistry.Elsevier Science,3:1-64.doi:10.1016/b0-08-043751-6/03016-4
Samson,S.D.,Hibbard,J.P.,Wort man,G.L.,1995.Ndisotopic evidence For juvenile crust in the Carolina ter-rane,southern Appalachians.Contributionsto Mineralo-gy and Petrology,121(2):171-184.doi:10.1007/s004100050097
Samson,S.D.,McClelland,W.C.,Patchett,P.J.,et al.,1989.Evidence from neodymium isotopes for mantlecontributions to Phanerozoic crustal genesis in theCanadian Cordillera.Nature,337:705-709.doi:10.1038/337705a0
Scherer,E.,Munker,C.,Mezger,K.,2001.Calibration ofthe lutetium-hafnium clock.Science,293(5530):683-687.doi:10.1126/science.1061372
Shi,G.H.,Miao,L.C.,Zhang,F.Q.,et al.,2004.Emplace-ment age and tectonic implications of the Xilinhot A-type granite in Inner Mongolia,China.Chinese ScienceBulletin,49(7):723-729.doi:10.1360/03wd0436
Shao,J.A.,Han,Q.J.,Zhang,L.Q.,et al.,1999.Twokinds of vertical accretion of the continental crust:anexample of the Da Hinggan Mts..Acta Ptrologica Sin-ica,49(7):600-606(in Chinese with English ab-stract).
Song,B.,Nutman,A.P.,Liu,D.Y.,et al.,1996.3800to2500Ma crustal evolutionin the Anshan area of Liaoning Prov-ince,northeastern China.Precambrian Research,78(1-3):79-94.doi:10.1016/0301-9268(95)00070-4
Sun,D.Y.,Wu,F.Y.,Li,H.M.,et al.,2001.Emplacementage of the postorogenic A-type granites in northwesternLesser Xing an ranges,and its relationship to the east-ward extension of Suolushan-Hegenshan-Zhalaite colli-sional suture zone.Chinese Science Bulletin,46(5):428-433.
Taylor,S.R.,McLennan,S.M.,1985.Continental crust:itscomposition and evolution.Blackwell Scientific,Oxford,311.doi:10.1016/0031-9201(86)90093-2
Taylor,S.R.,McLennan,S.M.,1995.The geochemical evo-lution of the continental crust.Reviews of Geophysics,33(2):241-265.doi:10.1029/95rg00262
Taylor,S.R.,McLennan,S.M.,McCulloch,M.T.,1983.Geochemistry of loess,continental crustal compositionand crustal model ages.Geochimica et CosmochimicaActa,47(11):1897-1905.doi:10.1016/0016-7037(83)90206-5
Veevers,J.J.,Saeed,A.,Belousova,E.A.,et al.,2005.U-Pb ages and source composition by Hf-isotope andtrace-element analysis of detrital zircons in Permiansandstone and modemsand fromsouthwestern Austral-ia and a reviewof the paleogeographical and denudation-al history of the Yilgamcraton.Earth-Science Reviews,68(3-4):245-279.doi:10.1016/j.earscirev.2004.05.005
Vermeesch,P.,2004.How many grains are needed for aprovenance study Earth and Planetary Science Let-ters,224(3-4):441-451.doi:10.1016/j.cpsl.2004.05.037
Vervoort,J.D.,Patchett,P.J.,1996.Behavior of hafniumand neodymiumisotopes in the crust:constraints from Precambrian crustally derived granites.Geochimica etCosmochimica Acta,60(19):3717-3733.doi:10.1016/0016-7037(96)00201-3
Wang,L.,Kusky,T.M.,Li,S.Z.,2010.Structural geometryof an exhumed UHPterraneinthe eastern Sulu orogen,China:implications for continental collisional proces-ses.Journal of Structural Geology,32(4):423-444.doi:10.1016/j.jsg.2010.01.012
Wang,T.,Zheng,Y.D.,Li,T.B.,et al.,2004.Mesozoicgranitic magmatism in extensional tectonics near theMongolian border in China andits implications for crus-tal growth.Journal of Asian Earth Sciences,23(5):715-729.doi:10.1016/s1367-9120(03)00133-0
Watson,E.B.,Harrison,T.M.,2005.Zircon thermometerreveals minimum melting conditions on earliest Earth.Science,308(5723):841-844.doi:10.1126/science.1110873
Watson,E.B.,Wark,D.A.,Thomas,J.B.,2006.Crystalli-zation thermometers for zircon and rutile.Contributionsto Mineralogy and Petrology,151(4):413-433.doi:10.1007/s00410-006-0068-5
Weislogel,A.L.,Graham,S.A.,Chang,E.Z.,et al.,2006.Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex:sedimentary record of collision of theNorth and South China blocks.Geology,34(2):97-100.doi:10.1130/g21929
Woodhead,J.,Hergt,J.,Shelley,M.,et al.,2004.ZirconHf-isotope analysis with an excimer laser,depth profi-ling,ablation of complex geometries,and concomitantage estimation.Chemical Geology,209(1-2):121-135.doi:10.1016/j.chemgeo.2004.04.026
Wu,F.Y.,Jahn,B.M.,Wilde,S.,et al.,2000.Phanerozoiccrustal growth:U-Pb and Sr-Ndisotopic evidencefromthegranites in northeastern China.Tectonophysics,328(1-2):89-113.doi:10.1016/s0040-1951(00)00179-7
Wu,F.Y.,Jahn,B.M.,Wilde,S.A.,et al.,2003.Highlyfractionated I-type granites in NE China(I):geochro-nology and petrogenesis.Lithos,66(3-4):241-273.doi:10.1016/s0024-4937(02)00222-0
Wu,F.Y.,Sun,D.Y.,Li,H.M.,et al.,2002.A-type granitesin northeastern China:age and geochemical constraints ontheir petrogenesis.Chemical Geology,187(1-2):143-173.doi:10.1016/s0009-2541(02)00018-9
Wu,F.Y.,Zhao,G.C.,Sun,D.Y.,et al.,2007.The HulanGroup:its role in the evolution of the central Asianorogenic belt of NE China.Journal of Asian Earth Sci-ences,30(3-4):542-556.doi:10.1016/j.jseaes.2007.01.003
Wu,F.Y.,Zhao,G.C.,Wilde,S.A.,et al.,2005.Nd isotop-ic constraints on crustal formation in the North Chinacraton.Journal of Asian Earth Sciences,24(5):523-545.doi:10.1016/j.jseaes.2003.10.011
Xu,W.L.,Ji,W.Q.,Pei,F.P.,et al.,2009.Triassic volcan-ismin eastern Heilongjiang and Jilin Provinces,NE Chi-na:chronology,geochemistry,and tectonic implica-tions.Journal of Asian Earth Sciences,34(3):392-402.doi:10.1016/j.jseaes.2008.07.001
Yang,J.,Gao,S.,Chen,C.,et al.,2009.Episodic crustalgrowth of North China as revealed by U-Pb age and Hfisotopes of detrital zircons from modern rivers.Geochimicaet Cosmochimica Acta,73(9):2660-2673.doi:10.1016/j.gca.2009.02.007
Yang,J.,Gao,S.,Yuan,H.L.,et al.,2007.Detrital zirconages of Hanjiang River:constraints on evolution ofnorthern Yangtze craton,South China.Journal of Chi-na University of Geosciences,18(3):210-222.
Yin,A.,Nie,S.,1993.An indentation model for the Northand South China collision and the development of theTan-Lu and Honamfault systems,eastern Asia.Tecton-ics,12(4):801-813.doi:10.1029/93tc00313
Yuan,H.L.,Gao,S.,Dai,M.N.,et al.,2008.Simultaneousdeterminations of U-Pb age,Hf isotopes and trace ele-ment compositions of zircon by excimer laser-ablationquadrupole and multiple-collector ICP-MS.ChemicalGeology,247(1-2):100-118.doi:10.1016/j.chem-geo.2007.10.003
Yuan,H.L.,Gao,S.,Liu,X.M.,et al.,2004.Accurate U-Pb age and trace element determinations of zircon byla-ser ablation-inductively coupled plasma-mass spectrom-etry.Geostandards and Geoanalytical Research,28(3):353-370.doi:10.1111/j.1751-908x.2004.tb00755.x
Zhai,M.G.,Gong,B.L.,Guo,J.H.,et al.,2000.Sm-Nd ge-ochronology and petrography of garnet pyroxene granu-lites in the northern Sulu region of China and their geo-tectonic implication.Lithos,52(1-4):23-33.doi:10.1016/s0024-4937(99)00082-1
Zhang,C.L.,Gao,S.,Zhang,G.W.,et al.,2003.Geochem-istry of Early Paleozoic alkali dyke swarms in southQinling and its geological significance.Science in China(Series D),46(12):1292-1306.doi:10.1360/03yd0520
Zhang,S.H.,Zhao,Y.,Song,B.,et al.,2007.Carboniferousgranitic plutons fromthe northern margin of the NorthChina block:implications for a Late Palaeozoic activecontinental margin.Journal of the Geological Society,164:451-463.doi:10.1144/0016-76492005-190
Zhang,X.H.,Zhang,H.F.,Tang,Y.J.,et al.,2008.Geo-chemistry of Permian bimodal volcanic rocks fromcen-tral Inner Mongolia,North China:implication for tec-tonic setting and Phanerozoic continental growthin cen-tral Asian orogenic belt.Chemical Geology,249(3-4):262-281.doi:10.1016/j.chemgeo.2008.01.005
Zhao,G.C.,Cawood,P.A.,Wilde,S.A.,et al.,2000.Meta-morphismof basement rocks in the central zone of theNorth China craton:implications for Paleoproterozoictectonic evolution.Precambrian Research,103(1-2):55-88.doi:10.1016/s0301-9268(00)00076-0
Zhao,G.C.,Sun,M.,Wilde,S.A.,et al.,2005.Late ArcheantoPaleoproterozoic evolution of the North China craton:keyissues revisited.Precambrian Research,136(2):177-202.doi:10.1016/j.precamres.2004.10.002
Zhao,G.C.,Wilde,S.A.,Cawood,P.A.,et al.,1998.Ther-mal evolution of Archean basement rocks fromthe east-ern part of the North China carton and its bearing ontectonic setting.International Geology Review,40(8):706-721.doi:10.1080/00206819809465233
Zhao,G.C.,Wilde,S.A.,Cawood,P.A.,et al.,1999.Ther-mal evolution of two textural types of mafic granulitesin the North China craton:evidence for both mantleplume and collisional tectonics.Geological Magazine,136(3):223-240.
Zhao,G.C.,Wilde,S.A.,Cawood,P.A.,et al.,2001.Ar-chean blocks and their boundaries in the North Chinacraton:lithological,geochemical,structural andP-Tpath constraints and tectonic evolution.PrecambrianResearch,107(1-2):45-73.doi:10.1016/s0301-9268(00)00154-6
Zhou,T.F.,Yuan,F.,Fan,Y.,et al.,2008.Granites in theSawuer region of the West Junggar,Xinjiang Province,China:geochronological and geochemical characteristicsand their geodynamic significance.Lithos,106(3-4):191-206.doi:10.1016/j.lithos.2008.06.014
程瑞玉,吴福元,葛文春,等,2006.黑龙江省东部饶河杂岩的就位时代与东北东部中生代构造演化.岩石学报,22(2):353-376.
葛文春,吴福元,周长勇,等,2005.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义.岩石学报,21(3):749-762.
邵济安,韩庆军,张履桥,等,1999.陆壳垂向增生的两种方式:以大兴安岭为例.岩石学报,15(4):600-606.
Bichert-Toft,J.,Albarède,F.,1997.The Lu-Hf isotope geo-chemistry of chondrites and the evolution of the mantle-crust system.Earth and Planetary Science Letters,148(1-2):243-258.doi:10.1016/s0012-821x(97)00040-x
Campbell,I.H.,Allen,C.M.,2008.Formation of supercon-tinents linked to increases in at mospheric oxygen.Na-ture Geoscience,1(8):554-558.doi:10.1038/ngeo259
Cawood,P.A.,Nemchin,A.A.,Strachan,R.,et al.,2007.Sedimentary basin and detrital zircon record along EastLaurentia and Baltica during assembly and breakup ofRodinia.Journal ofthe Geological Society,164(2):257-275.doi:10.1144/0016-76492006-115
Chen,B.,Jahn,B.M.,Tian,W.,2009.Evolution of the So-lonker suture zone:constraints fromzircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compo-sitions of subduction-and collision-related magmas andforearc sediments.Journal of Asian Earth Sciences,34(3):245-257.doi:10.1016/j.jseaes.2008.05.007
Chen,B.,Jahn,B.M.,Wilde,S.,et al.,2000.Two contras-ting paleozoic magmatic belts in northern Inner Mongo-lia,China:petrogenesis and tectonic implications.Tec-tonophysics,328(1-2):157-182.doi:10.1016/s0040-1951(00)00182-7
Cheng,R.Y.,Wu,F.Y.,Ge,W.C.,et al.,2006.Emplace-ment age of the Raohe complex in eastern HeilongjiangProvince and the tectonic evolution of the eastern partof northeastern China.Acta Petrologica Sinica,22(2):353-376(in Chinese with English abstract).
Chu,N.C.,Taylor,R.N.,Chavagnac,V.,et al.,2002.Hfisotope ratio analysis using multi-collector inductivelycoupled plasma mass spectrometry:an evaluation ofisobaric interference corrections.Journal of AnalyticalAtomic Spectrometry,17(12):1567-1574.doi:10.1039/b206707b
Condie,K.C.,1998.Episodic continental growth and super-continents:a mantle avalanche connection Earth andPlanetary Science Letters,163(1-4):97-108.doi:10.1016/s0012-821x(98)00178-2
Condie,K.C.,2000.Episodic continental growth models:af-terthoughts and extensions.Tectonophysics,322(1-2):153-162.doi:10.1016/s0040-1951(00)00061-5
Condie,K.C.,Aster,R.C.,2010.Episodic zircon age spectraof orogenic granitoids:the supercontinent connectionand continental growth.Precambrian Research,180(3-4):227-236.doi:10.1016/j.precamres.2010.03.008
Condie,K.C.,Belousova,E.,Griffin,W.L.,et al.,2009.Gran-itoid events in space and time:constraints fromigneous anddetrital zircon age spectra.Gondwana Research,15(3-4):228-242.doi:10.1016/j.gr.2008.06.001
Condie,K.C.,Beyer,E.,Belousova,E.,et al.,2005.U-Pbisotopic ages and Hf isotopic composition of single zir-cons:the search for juvenile Precambrian continentalcrust.Precambrian Research,139(1-2):42-100.doi:10.1016/j.precamres.2005.04.006
Coogan,L.A.,Hinton,R.W.,2006.Do the trace element com-positions of detrital zircons require Hadean continentalcrust Geology,34(8):633-636.doi:10.1130/g22737
De Bieve,P.,Taylor,P.D.P.,1993.Table of the isotopiccomposition of elements.International Journal of MassSpectrometryIon and Process,123:149-166.doi:10.1016/0168-1176(93)87009-h
DePaolo,D.J.,Linn,A.M.,Schubert,G.,1991.The conti-nental crustal age distribution:methods of determiningmantle separation ages from Sm-Nd isotopic data andapplicatoin to the southwestern United States.Journalof Geophysical Research,96(B2):2071-2088.doi:10.1029/90jb02219
Fan,W.M.,Guo,F.,Wang,Y.J.,et al.,2003.Late Meso-zoic calc-alkaline volcanism of post-orogenic extensionin the northern Dahinggan Mountains,northeasternChina.Journal of Volcanology and Geothermal Re-search,121(1-2):115-135.doi:10.1016/s0377-0273(02)00415-8
Faure,M.,Lin,W.,Le Breton,N.,2001.Where is the NorthChina-South China block boundary in eastern China.Geology,29(2):119-122.doi:10.1130/0091-7613(2001)029<0119
Ferry,J.M.,Watson,E.B.,2007.Newthermodynamic mod-els and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers.Contributions to Mineralogyand Petrology,154(4):429-437.doi:10.1007/s00410-007-0201-0
Gao,S.,Rudnick,R.L.,Carlson,R.W.,et al.,2002.Re-Osevidence for replacement of ancient mantle lithospherebeneath the North China craton.Earth and PlanetaryScience Letters,198(3-4):307-322.doi:10.1016/s0012-821x(02)00489-2
Gao,S.,Rudnick,R.L.,Yuan,H.L.,et al.,2004.Recyclinglower continental crust in the North China craton.Na-ture,432(7019):892-897.doi:10.1038/nature03162
Gao,S.,Zhang,J.F.,Xu,W.L.,et al.,2009.Delaminationand destruction of the North China craton.Chinese Sci-ence Bulletin,54(19):3367-3378.doi:10.1007/s11434-009-0395-9
Ge,W.C.,Wu,F.Y.,Zhou,C.Y.,et al.,2005.Zircon U-Pbages and its significance of the Mesozoic granites in theWulanhaote region,Central Da Hinggan Mountain.ActaPetrologica Sinica,21(3):749-762(in Chinese withEnglish abstract).
Gilder,S.A.,Leloup,P.H.,Courtillot,V.,et al.,1999.Tectonic evolution of the Tancheng-Lujiang(Tan-Lu)fault via Middle Triassic to Early Cenozoic paleomag-netic data.Journal of Geophysical Research-SolidEarth,104(B7):15365-15390.doi:10.1029/1999jb900123
Goldschmidt,V.M.,1933.Grundlagen der quantitativen geo-chemie.Fortschritte der Mineralogic KirstlographiePetrographie,17:112.
Griffin,W.L.,Belousova,E.A.,Shee,S.R.,et al.,2004.Archean crustal evolution in the northern Yilgam cra-ton:U-Pb and Hf-isotope evidence from detrital zir-cons.Precambrian Research,131(3-4):231-282.doi:10.1016/j.precamres.2003.12.011
Hacker,B.R.,Wallis,S.R.,Mc Williams,M.O.,et al.,2009.40Ar/39Ar constraints on the tectonic history andarchitecture of the ultrahigh-pressure Sulu orogen.Journal of Metamorphic Geology,27(9):827-844.doi:10.1111/j.1525-1314.2009.00840.x
Hanchar,J.M.,Hoskin,P.W.O.,2003.Zircon:reviews inmineralogy and geochemistry.Mineralogical Society ofAmerica,53:500.
Hawkesworth,C.J.,Dhuime,B.,Pietranik,A.B.,et al.2010.The generation and evolution of the continentalcrust.Journal ofthe Geological Society,167(2):229-248.doi:10.1144/0016-76492009-072
Hawkesworth,C.J.,Kemp,A.I.S.,2006a.Evolution of thecontinental crust.Nature,443(7113):811-817.doi:10.1038/nature05191
Hawkesworth,C.J.,Kemp,A.I.S.,2006b.Using hafniumand oxygenisotopes in zircons to unravel the record ofcrustal evolution.Chemical Geology,226(3-4):144-162.doi:10.1016/j.chemgeo.2005.09.018
Hu,Z.C.,Gao,S.,2008.Upper crustal abundances of trace ele-ments:a revision and update.Chemical Geology,253(3-4):205-221.doi:10.1016/j.chemgeo.2008.05.010
Iizuka,T.,Hirata,T.,2005.Improvements of precision andaccuracy in in situ Hf isotope microanalysis of zirconusing the laser ablation-MC-ICPMS technique.Chemi-cal Geology,220(1-2):121-137.doi:10.1016/j.chemgeo.2005.03.010
Iizuka,T.,Hirata,T.,Komiya,T.,et al.,2005.U-Pb andLu-Hf isotope systematics of zircons from the Missis-sippi River sand:implications for reworking and growthof continental crust.Geology,33(6):485-488.doi:10.1130/g21427.1
Jackson,S.E.,Pearson,N.J.,Griffin,W.L.,et al.,2004.The application of laser ablation-inductively coupledplasma-mass spectrometry to in situ U-Pb zircon geo-chronology.Chemical Geology,211(1-2):47-69.doi:10.1016/j.chemgeo.2004.06.017
Jahn,B.M.,Capdevila,R.,Liu,D.Y.,et al.,2004.Sourcesof Phanerozoic granitoids in the transect Bayanhongor-Ulaan Baatar,Mongolia:geochemical and Nd isotopicevidence,and implications for Phanerozoic crustalgrowth.Journal of Asian Earth Sciences,23(5):629-653.doi:10.1016/s1367-9120(03)00125-1
Jahn,B.M.,Wu,F.Y.,Capdevila,R.,et al.,2001.Highlyevolved juvenile granites with tetrad REE patterns:theWoduhe and Baerzhe granites from the Great Xing anMountains in NE China.Lithos,59(4):171-198.doi:10.1016/s0024-4937(01)00066-4
Jahn,B.M.,Wu,F.Y.,Chen,B.,2000a.Granitoids of theCentral Asian orogenic belt and continental growth inthe Phanerozoic.Transactions of the Royal Society ofEdinburgh:Earth and Environmental Sciences,350:181-193.doi:10.1130/0-8137
Jahn,B.M.,Wu,F.Y.,Hong,D.W.,2000b.Importantcrustal growth in the Phanerozoic:isotopic evidence ofgranitoids from East-Central Asia.Proceedings of theIndian Academy of Sciences-Earth and Planetary Sci-ences,109(1):5-20.doi:10.1007/bf02719146
Jian,P.,Liu,D.Y.,Kroner,A.,et al.,2008.Time scale ofan early to Mid-Paleozoic orogenic cycle of the long-lived Central Asian orogenic belt,Inner Mongolia ofChina:implications for continental growth.Lithos,101(3-4):233-259.doi:10.1016/j.lithos.2007.07.005
Kemp,A.I.S.,Hawkesworth,C.J.,Paterson,B.A.,et al.,2006.Episodic growth of the Gondwana supercontinentfrom hafnium and oxygen isotopes in zircon.Nature,439(7076):580-583.doi:10.1038/nature04505
Kusky,T.M.,Santosh,M.,2009.The Columbia connectionin North China.Geological Society of London:SpecialPublications,323:49-71.doi:10.1144/sp323.3
Li,S.Z.,Kusky,T.M.,Liu,X.C.,et al.,2009.Two-stage col-lision-related extrusion of the western Dabie HP-UHPmetamorphic terranes,Central China:evidence fromquartzc-axis fabrics and structures.Gondwana Research,16(2):294-309.doi:10.1016/j.gr.2009.03.003
Li,X.H.,Li,Z.X.,Ge,W.C.,et al.,2003.Neoproterozoicgranitoids in South China:crustal melting above a mantleplume at ca.825Ma.Precambrian Research,122(1-4):45-83.doi:10.1016/s0301-9268(02)00207-3
Li,X.H.,Li,Z.X.,Zhou,H.W.,et al.,2002.U-Pb zircongeochronology,geochemistry and Nd isotopic study ofNeoproterozoic bimodal volcanic rocks in the KangdianRift of South China:implications for the initial riftingof Rodinia.Precambrian Research,113(1-2):135-154.doi:10.1016/s0301-9268(01)00207-8
Li,Z.X.,1994.Collision between the North and South Chinablocks:a crustal-detachment model for suturinginthe regioneast of the Tanlu fault.Geology,22(8):739-742.doi:10.1130/0091-7613(1995)023<0574:cbtnas>2.3.CO
Liu,D.Y.,Nut man,A.P.,Compston,W.,et al.,1992.Remnants of≥3800Ma crust inthe Chinese part of theSino-Korean craton.Geology,20(4):339-342.doi:10.1130/0091-7613(1992)020<0339:romcit>2.3.CO
Liu,W.,Siebel,W.,Li,X.J.,et al.,2005.Petrogenesis of theLinxi granitoids,northern Inner Mongolia of China:con-straints on basaltic underplating.Chemical Geology,219(1-4):5-35.doi:10.1016/j.chemgeo.2005.01.013
Liu,X.M.,Gao,S.,Di wu,C.R.,et al.,2008.Precambriancrustal growth of Yangtze craton as revealed by detritalzircon studies.American Journal of Science,308(4):421-468.doi:10.2475/04.2008.02
Ludwig,K.R.,2003.ISOPLOT3:a geochronological toolkitfor Microsoft Excel.Berkeley Geochronology CentreSpecial Publication,Berkeley,California,70.
McLennan,S.M.,2001.Relationships between the trace ele-ment composition of sedimentary rocks and upper conti-nental crust.Geochemistry Geophysics Geosystems,2(4):1021-1044.doi:10.1029/2000gc000109
Meng,F.X.,Gao,S.,Yuan,H.L.,et al.,2010.Permian-tri-assic(260-220Ma)crustal growth of eastern centralAsian orogenic belt as revealed by detrital zircon stud-ies.American Journal of Science,310(5):364-404.doi:10.2475/05.2010.02
Meng,Q.R.,Zhang,G.W.,2000.Geologic framework andtectonic evolution of the Qinling orogen,central China.Tectonophysics,323(3-4):183-196.doi:10.1016/s0040-1951(00)00106-2
Miao,L.C.,Fan,W.M.,Liu,D.Y.,et al.,2008.Geochro-nology and geochemistry of the Hegenshan ophioliticcomplex:implications for late-stage tectonic evolutionof the Inner Mongolia-Daxinganling orogenic belt,Chi-na.Journal of Asian Earth Sciences,32(5-6):348-370.doi:10.1016/j.jseaes.2007.11.005
Oh,C.W.,Kusky,T.,2007.The Late Permian to TriassicHongseong-odesan collision belt in South Korea,anditstectonic correlation with China and Japan.InternationalGeology Review,49(7):636-657.doi:10.2747/0020-6814.49.7.636
Okay,A.I.,Seng r,A.M.C.,1992.Evidence for intraconti-nental thrust-related exhumation of the ultra-high-pres-sure rocks in China.Geology,20(5):411-414.doi:10.1130/0091-7613(1992)020<0411:efitre>2.3.CO
Pietranik,A.B.,Hawkesworth,C.J.,Storey,C.D.,et al.,2008.Episodic,mafic crust formation from4.5to2.8Ga:new evidence from detrital zircons,Slave craton,Canada.Geology,36(11):875-878.doi:10.1130/g24861a.1
Rudnick,R.L.,Gao,S.,2003.Composition of the continentalcrust:the crust:treatise on geochemistry.Elsevier Science,3:1-64.doi:10.1016/b0-08-043751-6/03016-4
Samson,S.D.,Hibbard,J.P.,Wort man,G.L.,1995.Ndisotopic evidence For juvenile crust in the Carolina ter-rane,southern Appalachians.Contributionsto Mineralo-gy and Petrology,121(2):171-184.doi:10.1007/s004100050097
Samson,S.D.,McClelland,W.C.,Patchett,P.J.,et al.,1989.Evidence from neodymium isotopes for mantlecontributions to Phanerozoic crustal genesis in theCanadian Cordillera.Nature,337:705-709.doi:10.1038/337705a0
Scherer,E.,Munker,C.,Mezger,K.,2001.Calibration ofthe lutetium-hafnium clock.Science,293(5530):683-687.doi:10.1126/science.1061372
Shi,G.H.,Miao,L.C.,Zhang,F.Q.,et al.,2004.Emplace-ment age and tectonic implications of the Xilinhot A-type granite in Inner Mongolia,China.Chinese ScienceBulletin,49(7):723-729.doi:10.1360/03wd0436
Shao,J.A.,Han,Q.J.,Zhang,L.Q.,et al.,1999.Twokinds of vertical accretion of the continental crust:anexample of the Da Hinggan Mts..Acta Ptrologica Sin-ica,49(7):600-606(in Chinese with English ab-stract).
Song,B.,Nutman,A.P.,Liu,D.Y.,et al.,1996.3800to2500Ma crustal evolutionin the Anshan area of Liaoning Prov-ince,northeastern China.Precambrian Research,78(1-3):79-94.doi:10.1016/0301-9268(95)00070-4
Sun,D.Y.,Wu,F.Y.,Li,H.M.,et al.,2001.Emplacementage of the postorogenic A-type granites in northwesternLesser Xing an ranges,and its relationship to the east-ward extension of Suolushan-Hegenshan-Zhalaite colli-sional suture zone.Chinese Science Bulletin,46(5):428-433.
Taylor,S.R.,McLennan,S.M.,1985.Continental crust:itscomposition and evolution.Blackwell Scientific,Oxford,311.doi:10.1016/0031-9201(86)90093-2
Taylor,S.R.,McLennan,S.M.,1995.The geochemical evo-lution of the continental crust.Reviews of Geophysics,33(2):241-265.doi:10.1029/95rg00262
Taylor,S.R.,McLennan,S.M.,McCulloch,M.T.,1983.Geochemistry of loess,continental crustal compositionand crustal model ages.Geochimica et CosmochimicaActa,47(11):1897-1905.doi:10.1016/0016-7037(83)90206-5
Veevers,J.J.,Saeed,A.,Belousova,E.A.,et al.,2005.U-Pb ages and source composition by Hf-isotope andtrace-element analysis of detrital zircons in Permiansandstone and modemsand fromsouthwestern Austral-ia and a reviewof the paleogeographical and denudation-al history of the Yilgamcraton.Earth-Science Reviews,68(3-4):245-279.doi:10.1016/j.earscirev.2004.05.005
Vermeesch,P.,2004.How many grains are needed for aprovenance study Earth and Planetary Science Let-ters,224(3-4):441-451.doi:10.1016/j.cpsl.2004.05.037
Vervoort,J.D.,Patchett,P.J.,1996.Behavior of hafniumand neodymiumisotopes in the crust:constraints from Precambrian crustally derived granites.Geochimica etCosmochimica Acta,60(19):3717-3733.doi:10.1016/0016-7037(96)00201-3
Wang,L.,Kusky,T.M.,Li,S.Z.,2010.Structural geometryof an exhumed UHPterraneinthe eastern Sulu orogen,China:implications for continental collisional proces-ses.Journal of Structural Geology,32(4):423-444.doi:10.1016/j.jsg.2010.01.012
Wang,T.,Zheng,Y.D.,Li,T.B.,et al.,2004.Mesozoicgranitic magmatism in extensional tectonics near theMongolian border in China andits implications for crus-tal growth.Journal of Asian Earth Sciences,23(5):715-729.doi:10.1016/s1367-9120(03)00133-0
Watson,E.B.,Harrison,T.M.,2005.Zircon thermometerreveals minimum melting conditions on earliest Earth.Science,308(5723):841-844.doi:10.1126/science.1110873
Watson,E.B.,Wark,D.A.,Thomas,J.B.,2006.Crystalli-zation thermometers for zircon and rutile.Contributionsto Mineralogy and Petrology,151(4):413-433.doi:10.1007/s00410-006-0068-5
Weislogel,A.L.,Graham,S.A.,Chang,E.Z.,et al.,2006.Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex:sedimentary record of collision of theNorth and South China blocks.Geology,34(2):97-100.doi:10.1130/g21929
Woodhead,J.,Hergt,J.,Shelley,M.,et al.,2004.ZirconHf-isotope analysis with an excimer laser,depth profi-ling,ablation of complex geometries,and concomitantage estimation.Chemical Geology,209(1-2):121-135.doi:10.1016/j.chemgeo.2004.04.026
Wu,F.Y.,Jahn,B.M.,Wilde,S.,et al.,2000.Phanerozoiccrustal growth:U-Pb and Sr-Ndisotopic evidencefromthegranites in northeastern China.Tectonophysics,328(1-2):89-113.doi:10.1016/s0040-1951(00)00179-7
Wu,F.Y.,Jahn,B.M.,Wilde,S.A.,et al.,2003.Highlyfractionated I-type granites in NE China(I):geochro-nology and petrogenesis.Lithos,66(3-4):241-273.doi:10.1016/s0024-4937(02)00222-0
Wu,F.Y.,Sun,D.Y.,Li,H.M.,et al.,2002.A-type granitesin northeastern China:age and geochemical constraints ontheir petrogenesis.Chemical Geology,187(1-2):143-173.doi:10.1016/s0009-2541(02)00018-9
Wu,F.Y.,Zhao,G.C.,Sun,D.Y.,et al.,2007.The HulanGroup:its role in the evolution of the central Asianorogenic belt of NE China.Journal of Asian Earth Sci-ences,30(3-4):542-556.doi:10.1016/j.jseaes.2007.01.003
Wu,F.Y.,Zhao,G.C.,Wilde,S.A.,et al.,2005.Nd isotop-ic constraints on crustal formation in the North Chinacraton.Journal of Asian Earth Sciences,24(5):523-545.doi:10.1016/j.jseaes.2003.10.011
Xu,W.L.,Ji,W.Q.,Pei,F.P.,et al.,2009.Triassic volcan-ismin eastern Heilongjiang and Jilin Provinces,NE Chi-na:chronology,geochemistry,and tectonic implica-tions.Journal of Asian Earth Sciences,34(3):392-402.doi:10.1016/j.jseaes.2008.07.001
Yang,J.,Gao,S.,Chen,C.,et al.,2009.Episodic crustalgrowth of North China as revealed by U-Pb age and Hfisotopes of detrital zircons from modern rivers.Geochimicaet Cosmochimica Acta,73(9):2660-2673.doi:10.1016/j.gca.2009.02.007
Yang,J.,Gao,S.,Yuan,H.L.,et al.,2007.Detrital zirconages of Hanjiang River:constraints on evolution ofnorthern Yangtze craton,South China.Journal of Chi-na University of Geosciences,18(3):210-222.
Yin,A.,Nie,S.,1993.An indentation model for the Northand South China collision and the development of theTan-Lu and Honamfault systems,eastern Asia.Tecton-ics,12(4):801-813.doi:10.1029/93tc00313
Yuan,H.L.,Gao,S.,Dai,M.N.,et al.,2008.Simultaneousdeterminations of U-Pb age,Hf isotopes and trace ele-ment compositions of zircon by excimer laser-ablationquadrupole and multiple-collector ICP-MS.ChemicalGeology,247(1-2):100-118.doi:10.1016/j.chem-geo.2007.10.003
Yuan,H.L.,Gao,S.,Liu,X.M.,et al.,2004.Accurate U-Pb age and trace element determinations of zircon byla-ser ablation-inductively coupled plasma-mass spectrom-etry.Geostandards and Geoanalytical Research,28(3):353-370.doi:10.1111/j.1751-908x.2004.tb00755.x
Zhai,M.G.,Gong,B.L.,Guo,J.H.,et al.,2000.Sm-Nd ge-ochronology and petrography of garnet pyroxene granu-lites in the northern Sulu region of China and their geo-tectonic implication.Lithos,52(1-4):23-33.doi:10.1016/s0024-4937(99)00082-1
Zhang,C.L.,Gao,S.,Zhang,G.W.,et al.,2003.Geochem-istry of Early Paleozoic alkali dyke swarms in southQinling and its geological significance.Science in China(Series D),46(12):1292-1306.doi:10.1360/03yd0520
Zhang,S.H.,Zhao,Y.,Song,B.,et al.,2007.Carboniferousgranitic plutons fromthe northern margin of the NorthChina block:implications for a Late Palaeozoic activecontinental margin.Journal of the Geological Society,164:451-463.doi:10.1144/0016-76492005-190
Zhang,X.H.,Zhang,H.F.,Tang,Y.J.,et al.,2008.Geo-chemistry of Permian bimodal volcanic rocks fromcen-tral Inner Mongolia,North China:implication for tec-tonic setting and Phanerozoic continental growthin cen-tral Asian orogenic belt.Chemical Geology,249(3-4):262-281.doi:10.1016/j.chemgeo.2008.01.005
Zhao,G.C.,Cawood,P.A.,Wilde,S.A.,et al.,2000.Meta-morphismof basement rocks in the central zone of theNorth China craton:implications for Paleoproterozoictectonic evolution.Precambrian Research,103(1-2):55-88.doi:10.1016/s0301-9268(00)00076-0
Zhao,G.C.,Sun,M.,Wilde,S.A.,et al.,2005.Late ArcheantoPaleoproterozoic evolution of the North China craton:keyissues revisited.Precambrian Research,136(2):177-202.doi:10.1016/j.precamres.2004.10.002
Zhao,G.C.,Wilde,S.A.,Cawood,P.A.,et al.,1998.Ther-mal evolution of Archean basement rocks fromthe east-ern part of the North China carton and its bearing ontectonic setting.International Geology Review,40(8):706-721.doi:10.1080/00206819809465233
Zhao,G.C.,Wilde,S.A.,Cawood,P.A.,et al.,1999.Ther-mal evolution of two textural types of mafic granulitesin the North China craton:evidence for both mantleplume and collisional tectonics.Geological Magazine,136(3):223-240.
Zhao,G.C.,Wilde,S.A.,Cawood,P.A.,et al.,2001.Ar-chean blocks and their boundaries in the North Chinacraton:lithological,geochemical,structural andP-Tpath constraints and tectonic evolution.PrecambrianResearch,107(1-2):45-73.doi:10.1016/s0301-9268(00)00154-6
Zhou,T.F.,Yuan,F.,Fan,Y.,et al.,2008.Granites in theSawuer region of the West Junggar,Xinjiang Province,China:geochronological and geochemical characteristicsand their geodynamic significance.Lithos,106(3-4):191-206.doi:10.1016/j.lithos.2008.06.014
程瑞玉,吴福元,葛文春,等,2006.黑龙江省东部饶河杂岩的就位时代与东北东部中生代构造演化.岩石学报,22(2):353-376.
葛文春,吴福元,周长勇,等,2005.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义.岩石学报,21(3):749-762.
邵济安,韩庆军,张履桥,等,1999.陆壳垂向增生的两种方式:以大兴安岭为例.岩石学报,15(4):600-606.
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