72

彭卓伦,RodneyGrapes,庄文明,等/

地学前缘(EarthScienceFrontiers)2011,18(1)

formation:EvidencefromSEChina[J].InternationalGeolo-gyReview,2003,45:611-622.

[11] ChenGN,GrapesRH,ZhangK.Mesozoiccrustalmelting

andtectonicdeformationinSEChina[J].InternationalGeol-ogyReview,2003,45(10):948-957.

[12] ChenGN,GrapesR.GraniteGenesis:In-situMeltingand

CrustalEvolution[M].Dordrecht,Netherlands:Springer,2007.

[13] 周新民,姚玉鹏,徐夕生.浙东大衢山花岗岩中淬冷包体及

其成因机制[J].岩石学报,1992,8(3):234-242.

[14] 杜杨松.酸性-中酸性火山-侵入杂岩中岩石包体研究的新进

展[J].现代地质,1996,10(2):169-174.

[15] 徐夕生,周新民.花岗岩类中的岩石包体[J].南京大学学

报:地球科学版,1988(1):234-241.

[16] ZhuoXM,LiWX.OriginofLateMesozoicigneousrocksin

southeasternChina:Implicationsforlithospheresubductionandunderplatingofmaficmagmas[J].2000,326:269-287.

[17] YangJH,WuFY,ChungSL,etal.AHybridoriginfor

theQianshanA-typegranite,northeastChina:GeochemicalandSr-Nd-Hfisotopicevidence[J].Lithos,2006,89:89-106.

[18] YangJH,WuFY,ChungSL,etal.Multiplesourcesfor

theoriginofgranites:GeochemicalandNd/Srisotopicev-idencefromtheGudaolinggraniteanditsmaficenclaves,northeastChina[J].GeochimicaetCosmochimicaActa,2004,21:4469-4483.

[19] RolandMAAS,NichollsIA,LeggC.Igneousandmeta-morphicenclavesintheS-typededdickgranodiorite,Lachlanfoldbelt,SEAustralia:Petrographic,geochemicalandNd-Srisotopicevidenceforcrustalmeltingandmagmamixing[J].JournalofPetrology,1997,38:815-841.

[20] EberzGW,Karlsruhe,NichollsIA,etal.Microgranitoid

enclavesfromtheswiftscreekplutonSE-Australia:Texturalandphysicalconstraintsonthenatureofmagmaminglingprocessesintheplutonicenvironment[J].GeologischeRund-schau,1988,77:713-736.

[21] ColeJW,GambleJA,BurtRM,etal.Mixingandming-lingintheevolutionofandesite-dacitemagmas:Evidencefromco-magmaticplutonenclaves,Taupovolcaniczone,NewZealand[J].Lithos,2001,59:25-46.

[22] FrostTP,MahoodGA.Field,chemicalandphysicalcon-straintsonmafic-felsicmagmainteractionintheLamarkGranodiorite,SierraNevada,California[J].GeologicalSocie-tyofAmericaBulletin,1987,99:272-291.

[23] ChappellBW,WhiteAJR,WybornD.Theimportanceof

residualsourcematerial(restite)ingranitepetrogenesis[J].JTectonophysics,

[24] ElburgMA.Evidenceofisotopicequilibrationbetweenm-i

crogranitoidenclavesandhostgranodiorite,Warburtongran-odiorite,LachlanFoldBelt,Australia[J].Lithos,1996,38:1-22.

[25] 陈国能,张珂,徐伟,等.华南中生代花岗岩岩石包体的成

因与分类[J].中山大学学报:自然科学版,1993,32:305-311.

[26] 陈国能.关于花岗岩岩石包体的成因及岩基的定位问题[J].

高校地质学报,1998,4(3):346-349.

[27] Garc a-MorenoO,CastroA,Corretg LG,etal.Dissolu-tionoftonaliticenclavesinascendinghydrousgraniticmag-mas:Anexperimentalstudy[J].Lithos,2006,45:66-78.[28] 彭卓伦.花岗岩中的非均一暗色微粒包体及其成因研究[D].

广州:中山大学,2006.

[29] 庄文明,陈绍前,黄友义.佛冈复式岩体地质地球化学特征

及其成岩源岩[J].广东地质,2000,15(3):1-12.[30] 孟良义.花岗岩与成矿[M].北京:科学出版社,1993.[31] BuschW,SchneiderG,MehnertKR.Initialmeltingatgrain

boundariesPartII:Meltinginrocksofgranodioritic,quartz-dioriticandtonaliticcomposition[J].N.Jahrbuchf.Miner-alogie.Monatshefte,1974,116:345-370.

[32] 曲晓明,王鹤年,饶冰.胶东群部分熔化实验及其对花岗岩

成因的指示[J].地球化学,2000,29(2):153-161.

[33] ElburgMA,NichollsIA,SieSH.Mineralogicalevidence

fortheoriginofmaficmicrogranularenclavesinS-typegran-itesandvolcanics[J].NuclearInstrumentsandMethodsinPhysicsResearchB,1995,104:464-469.

[34] NardiLVS,deLimaEF.Hybridizationofmaficmicrogran-ularenclavesintheLavrasGraniteComplex,southernBrazil[J].JournalofSouthAmericanEarthSciences,2000,13:67-78.

[35] MartinVM,HolnessMB,PyleDM.Texturalanalysisof

magmaticenclavesfromtheKameniIslands,

Santorini,

Greece[J].JournalofVolcanologyandGeothermalRe-search,2006,125:126-140.

[36] 刘成东,张文秦,莫宣学,等.东昆仑约格鲁岩体暗色微粒

包体特征及成因[J].地质通报,2002,21(11):729-744.[37] 潘贵,刘宝山,李仰春.伊春地区晚奥陶世花岗质岩石中闪

长质包体的成因[J].中国地质,2002,29(4):364-368.[38] 彭卓伦,陈国能,GrapesR.花岗岩暗色微粒包体中的水及

其在包体研究中的意义[J].中山大学学报:自然科学版,2008,47(1):118-120.

[39] 彭卓伦,陈国能,GrapesR.深圳王母岩体暗色微粒包体中

的蚀变矿物[J].矿物岩石地球化学通报,2007,26(增刊):116-117.

[40] 徐夕生,周新民,王德滋.花岗岩中的钾长石巨晶:以南岭

佛岗花岗质杂岩体中微斜长石巨晶为例[J].高校地质学报,8(: