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Late-NeoarcheanmagmatismandmetamorphismatthesoutheasternmarginoftheNorthChinaCratonandtheirtectonicimplications

An-DongWanga,∗,Yi-CanLiua,∗,Xiao-FengGua,Zhen-HuiHoua,BiaoSongbaCASKeyLaboratoryofCrust-MantleMaterialsandEnvironments,SchoolofEarthandSpaceSciences,UniversityofScienceandTechnologyofChina,Hefei230026,China

bBeijingSHRIMPCenter,InstituteofGeology,ChineseAcademyofGeologicalSciences,Beijing100037,China

articleinfoArticlehistory:Received21May2012Receivedinrevisedform28July2012Accepted30July2012Available online xxxKeywords:ZirconU–PbdatingHfisotopeLate-NeoarcheanmagmatismandmetamorphismCrustalgrowthNorthChinaCratonabstractInthepresentstudy,twogneissxenolithsfromtheMesozoicJiagouintrusionatthesoutheasternmarginoftheNorthChinaCraton(NCC)areexaminedforinsituzirconSHRIMPU–PbdatingincombinationwithzircontraceelementandHfisotopeanalyses.Cathodoluminescence(CL)imagesandtraceelementdatarevealthatmostzirconsfromthedatedsamplesdisplaydistinctcore–rimstructures,i.e.,magmaticcores

andmetamorphicrims.Thecoresshowtypicaligneouscharacteristicswithoscillatorygrowthzoningandhighrareearthelement(REE)contents,whereasthemetamorphicrimsarecharacterizedbysphericaltoovalshape,andhighandhomogeneousluminescentintensity.ZirconSHRIMPU–Pbdatingresultssuggest

thatthexenolithsformedat2.55–2.64Gaandexperiencedhigh-grademetamorphismat2.48–2.49Ga.ThelowerHREEcontents,negativeEuanomalies,highTh/Uratios(generally>0.5)andhighTi-in-zircontemperatures(>800◦C)ofmetamorphiczirconrimssuggestthatthe2.48–2.49Gaeventrepresentsanepisodeofgranulitefaciesmetamorphism.Theseresultsdemonstratethatthelower-crustalrocksinthe

studiedareaexperiencedlate-Neoarcheanmagmatismandsubsequentmetamorphism.PositiveεHf(t)valuesof+2to+5,withmodelagesyoungerthan3.0Gaandformationagesof2.55–2.64Gaforigneouszirconsfromthexenolithsindicatethattheywerederivedfromjuvenilecrustalsourcesandstrongly

suggesttheexistenceofsignificantlate-Neoarcheancrustalgrowthintheregion.© 2012 Elsevier B.V. All rights reserved.

1.IntroductionEpisodicgrowthofjuvenilecontinentalcrusthasbeenrecog-nizedbyanumberofauthors(e.g.,McCullochandBennett,1994;Condie,1998),andearlyPrecambrianisregardedtobeacrucialstageforcontinentalcrustformation,occurringduringseveralpeakperiodssuchas3.6Ga,2.7Gaand1.8Ga(McCullochandBennett,1994;Condie,1998;Condieetal.,2011).However,insomePre-cambriancratonssuchastheNorthChinaCraton(NCC)andIndianShield,themajortectonothermaleventsoccurredextensivelyin2.5–2.6Ga(Clarketal.,2009;WangandLiu,2012andreferencestherein)andtheNeoarcheanhistoryofthesecratonsaremarkedlydifferentfromthatofmostothercratons.Inthepasttwodecades,greatachievementshavebeenmadeinunderstandingtheformationandevolutionoftheNCC.How-ever,thehistoryofcratonizationoftheNCCandthenatureoftectonothermaleventsarehighlycontroversial(e.g.,Zhaietal.,2000;Wildeetal.,2002;KuskyandLi,2003;Polatetal.,2005;Zhaoetal.,2005,2011;Gengetal.,2011;Nutmanetal.,2011;∗Correspondingauthors.Tel.:+865513600367;fax:+865513600367.E-mailaddresses:adw008@mail.ustc.edu.cn(A.-D.Wang),liuyc@ustc.edu.cn(Y.-C.Liu).Yingetal.,2011;ZhaiandSantosh,2011;Santoshetal.,2012a,b).AnimportantapproachtosolvethisdebateistoobtainmoregeochronologicalandgeochemicaldatarelatedtothePrecam-brianmagmatismandmetamorphismoverthecraton.WiththeaimtoavoidtheinfluenceoflategeologicalprocessesandthedisequilibriumofSr–Ndisotopesbetweenminerals,zirconcanberegardedasanidealmineralfordatingmultistagemagma-tismandmetamorphismofrocksinvolvedincomplexprocesses(e.g.,Y.C.Liuetal.,2011a).Asaconsequence,duetoitshighstabilityandclosuretemperature(Leeetal.,1997;CherniakandWatson,2000;GardésandMontel,2009)andtherapiddevelop-mentofinsitumicro-analyticaltechniquessuchasSHRIMPandLA-ICP-MSmethods,zirconhasbeenwidelyusedtodatevarious