引文
白文吉,杨经绥,Robinson,方青松,张仲明,颜秉刚,胡旭峰.2001.西藏罗布莎蛇绿岩铬铁矿中金刚石的研究.地质学报,75(3):404~409.
白文吉,杨经绥,施倪承,方青松,代明泉,熊明,颜秉刚.2004.西藏罗布莎蛇绿岩地幔岩中首次发现超高压矿物方铁矿和自然铁.地质论评,50(2):184~187.
白文吉,杨经绥,方青松,颜秉刚,张仲明,任玉峰,施倪承,马吉生,代明泉.2004.西藏蛇绿岩地幔中的主要自然金属矿物.地学前缘,11(1):179~187.
白文吉,杨经绥,方青松,颜秉刚,张仲明.2004.西藏罗布莎蛇绿岩豆荚状铬铁矿石中的合金成分.地质学报,78(5):676~682.
鲍学昭.1995.锆石中两种成分变化趋势及其成因标型意义.矿物学报,15:404~410.
鲍学昭,李惠民,陆松年.1998.锆石微区喇曼光谱研究及成因标型意义.地质科学,33(4):455~462.
陈道公,汪相,Deloule E,2001.北大别辉石岩成因:锆石微区年龄和化学组成.科学通报,46(7):586~590.
董申保,洪大卫,许保良.2001.花岗岩拓扑学的研究展望.地质论评,47(4):356~360.
杜远生,朱杰,韩欣,顾松竹.2004.从弧后盆地到前陆盆地——北祁连造山带奥陶纪—泥盆纪的沉积盆地与构造演化.地质通报,23(9~10):911~917.
樊祺诚,孙谦,李霓,隋建立.2004.琼北火山活动分期与全新世岩浆演化.岩石学报,20(3):533~544.
樊祺诚,孙谦,李霓,王团华.2005.镜泊湖全新世火山岩—岩浆的多样性.自然科学进展,15(8):943~950.
樊祺诚,隋建立,王团华,孙谦,李霓.2006.长白山天池火山粗面玄武岩的喷发历史与演化.岩石学报,22(6):1449~1457.
樊祺诚,孙谦,龙安明,尹克坚,隋建立,李霓,王团华.2006.北部湾涠洲岛及斜阳岛火山地质与喷发历史研究.岩石学报,22(6):1529~1537.
方春方,陈培荣.2000.赣南不同类型花岗岩体的锆石形态群特征及其意义.地质找矿论丛,15(4):299~306.
洪大卫.1995.碱性花岗岩的构造环境分类及其鉴别标志.中国科学(D辑),25:418~426.
简平,程裕淇,刘敦一.2001.变质锆石成因的岩相学研究——高级变质岩U-Pb年龄解释的基本依据.地学前缘,8(3):183~191.
金振民,高山.1996.底侵作用及其壳幔演化动力学意义,地质科技情报,15(2):1~7.
李献华,刘颖,涂相林,1996.S型花岗岩中锆石U-Pb同位素体系的多阶段演化及年代学意义.矿物学报,16(2):170~177.
林广春,马昌前.2003.过铝花岗岩的成因类型与构造环境研究综述.华南地质与矿产,1:65~70.
刘埃平,金景福.1996.牧护关花岗岩中锆石标型特征研究.地质地球化学,4:15~20.
刘显凡,卢秋霞.1997.锆石形态标型特征及标型生长机制探讨.矿物岩石杂志,16(2):179~184.
罗照华,柯珊,谌宏伟.2002.埃达克岩的特征、成因及构造意义.地质通报,21(7):436~440.
马昌前,王人镜,邱家骧.1992.花岗质岩浆起源和多次岩浆混合的标志:包体——以北京周口店岩体为例.地质论评,38(2):109~119.
马昌前.2003.造山岩套中镁铁质和长英质岩浆的相互作用研究进展.地质科技情报,22(3):1~8.
马昌前,明厚利,杨坤光.2004.大别山北麓的古生代岩浆弧:侵入岩年代学和地球化学证据.岩石学报,20(3):393~402.
苏建平,张新虎,胡能高,付国民,张海峰.2004b.中祁连西段野马南山埃达克质花岗岩的地球化学特征及成因.中国地质,31(4):365~371.
汤艳杰.2006.太行山地区中、新生代玄武质岩浆的源区特征与时空演化.岩石学报,22(6):1657~1664.
汪相,Pupin J P.1992.法国阿根特拉花岗岩中锆石的微量元素地球化学特征及地质意义.地质论评,12(3):260.
汪相.1998.锆石形态的定量描述及其动力学分析.中国科学(D辑),28(3):232~238.
汪相,Kienast J R.2000.微粒暗色包体中锆石的形态演化及其制约机制.中国科学(D辑),30(2):180~187.
汪相,李显武.2001.{211}型锆石的标型性研究.科学通报,46(17):1472~1476.
王德滋,周金城.1999.我国花岗岩研究的回顾与展望.岩石学报,15(2):161~69.
王德滋,沈渭洲.2003.中国东南部花岗岩成因与地壳演化.地学前缘,10(3):209~220.
王方正,杨梅珍,郑建平.2002.准噶尔盆地陆梁地区基底火山岩的岩石地球化学及其构造环境.岩石学报,18(1):9~16.
吴才来,杨经绥,Reland T,Wooden J L,李海兵,万渝生,史仁灯.2001.祁连南缘嗷唠山花岗岩SHRI MP锆石年龄及其地质意义.岩石学报,17(2):215~221.
吴才来,杨经绥;,杨宏仪,Wooden J L,史仁灯,陈松永,郑秋光.2004.北祁连东部两类I型花岗岩定年及其地质意义.岩石学报,20(3):425~432.
吴才来,杨经绥,姚尚志,曾令森、陈松永、李海兵、戚学祥.2005.北阿尔金巴什考供盆地南缘花岗杂岩体特征及锆石SHRI MP U-Pb定年.岩石学报,21(3):846~858.
吴才来,姚尚志,曾令森,杨经绥,Wooden J L,陈松永,Mazadab FK.2006.北祁连早古生代洋壳双向俯冲的花岗岩证据.中国地质,6:1197~1208.
谢桂青,胡瑞忠,蒋国豪,赵军红.2001.锆石的成因和U-Pb同位素定年的某些进展.地质地球化学,19(4):64~70.
许文良.1999.辽西中生代粗面玄武岩中地幔和下地壳捕虏体的发现及其地质意义.地质论评,45(增刊):444~449.
许文良,王冬艳,王清海,林景仟,刘晓春.2002.徐淮地区早侏罗世侵入杂岩体中榴辉岩类包体的发现及其地质意义.科学通报,(8):618~622.
许文良,王冬艳,王清海,林景仟.2003.鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学.岩石学报,19(4):623~636.
许文良,杨德彬,裴福萍,纪伟强.2005.辽东前任屯角闪岩形成的时代——锆石SHRI MP U-Pb定年证据.岩石矿物学杂志,24(4):273~278.
许志琴,徐惠芬,张建新,李海兵,朱志直,曲景川,陈代璋,陈金禄,杨开春.1994.北祁连走廊南山加里东俯冲杂岩增生地体及其动力学.地质学报,68(1):1~15.
徐夕生,周新民,王德滋.1999.壳幔作用与花岗岩成因——以中国东南沿海为例.高校地质学报,5(3):421~429.
杨经绥,白文吉,方青松,颜秉刚,施倪承,马哲生,代明泉,熊明.2002.蛇绿岩中的一种超高压矿物——硅金红石,12:1220~1222.
杨经绥,白文吉,方青松,颜秉刚,戎合,陈松永.2004.西藏罗布莎豆荚状铬铁矿中发现超高压矿物柯石英,地球科学,29:651~660.
杨经绥,白文吉,戎合,张仲明,许志琴,方青松,颜秉刚,李天福,任玉峰,陈松永.2005.中国大陆科学钻探(CCSD)主孔石榴子石橄榄岩中发现Fe-2P合金矿物.岩石学报,21:271~276.
杨岳衡.2006.华北克拉通中、新生代典型火山岩的岩石成因:Hf同位素新证据.岩石学报,22(6):1665~1671.
张宏福,英基丰,徐平,马玉光.2004.华北中生代玄武岩中地幔橄榄石捕虏晶:对岩石圈地幔置换过程的启示.科学通报,49(8):784~789.
张辉煌,徐义刚,葛文春,马金龙.2006.吉林伊通—大屯地区晚中生代—新生代玄武岩地球化学特征及其意义.岩石学报,22(6):1579~1596.
张旗,王焰,王元龙.2001.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约.岩石学报,17(4):505~513.
张旗,王焰,刘伟,王元龙.2002.埃达克岩的特征及其意义.地质通报,21(17):431~435.
张文慧,韩宝福.2006.内蒙古集宁新生代玄武岩的K-Ar年代学和地球化学及其深部动力学意义.岩石学报,22(6):1597~1607.
张招崇,王福生.2002.峨眉山大火成岩省中发现二叠纪苦橄质熔岩地质论评,48:448.
周新民,姚玉鹏,徐夕生.1992.浙东大巨山花岗岩中淬冷包体及其成因机制.岩石学报,8(3):234~242.
朱弟成,段丽萍,廖忠礼,潘桂棠.2002.两类埃达克岩(Adakite)的判别.矿物岩石,22(3):5~9.
Arnaud N O,Vidal P,Tapponnier P,Matt Ph and Deng W M.1992.The high volcanism of northwestern Tibet(Xizang):Geochemistry and tectonic i mplications.Earth and PlanetaryScience Letters,111:351~367.
Alvar S.2000.Fractional crystallization of mantle-derived melts as amechanismfor some I-type granite petrogenesis:an examplefrom Lachlan Fold Belt,Australia.London:Journal of theGeological Society,157:135~149.
Anthi L,Dieter G.1999.Constraining the prograde and retrogradeP—T—tpath of Eocene HP rocks by SHRI MP dating ofdifferent zircon domains:inferred rates of heating,burial,cooling and exhumation for central Rhodope,northern Greece.Contrib.Petrol.,135:340~354.
Armin Z,Williams I S,Helene B,Millar I L.2003.Different ageresponse of zircon and monazite during the tectono-matamorphic evolution of a high grade paragneiss from theRuhla Crystalline Comples,central Germany.Contrib.Petrol.,135:340~354.
Barbarin B.1999.A review of the relationships between granitoidtypes,their origins and their geodynamic environments.Lithos,46:605~626.
Barbey P,Alle P,Brouand M,Albarede F.1995.Rare-earth patterns in zircon from the Manslu granite and Tibetan Slabmigmatites(Hi malaya):insightsinthe origin and evolution of acrustally-derived granite magma.Chem Geol.,125:1~17.
Belousova E A,Griffin W L,Suzanne Y O,.2002.Igneouszircon:trace element composition as anindicator of source rocktype.Contrb.Petrol,143:602~622.
Bergantz G W.1989.Underplating and partial melting:i mplicationsfor melt generation and extraction.Science,245:1093~1094.
Bourdon B,Eissen J P,Monzier M,Robin C,Martin H,Cotton J,Hall.2002.Adakite-like lavas from Antisana volcano(Ecuador):Evidence for slab melt metasomatism beneath theAndem northern volcanic zone.Journal of Petrology,43:199~217.
Calvin F M,Susanne M Mand Russell W M.2003.Hot and coldgranites-I mplications of zircon saturation temperatures andpreservation of inheritance.Geology,31(6):529~532.
Castro A,Moreno-Ventas I and De la Rosa J D.1991.H-type(hybrid)granitoids:a proposed revision of the granite-typeclassification and nomenclature.Earth Science Reviews,31:237~253.
Chung S L and Jahn B.1995.Plume-lithosphere interaction ingeneration of the Emeishan flood basalts at the Permian—Triassic boundary.Geology,23:889~893.
Collins WJ.1996.S-and I-type granitoids of the eastern Lachlanfold belt:Products of three-component mixing.Transitions ofthe Royal Society of Edinburgh.Earth Sciences,88:171~179.
Collins W J.1998.Evolution of petrogenetic models for LachlanFold Belt granitoids:i mplications for crustal architecture andtectonic models.Australian Journal of Earth Sciences,45:483~500.
Defant MJ and Drummond MS.1990.Derivation of some modernarc magmas by melting of young subducted lithosphere.Nature,347:662~665.
Defant MJ,Kepezhinskas P.2001.Evidence suggests slab meltingin arc magmas.EOS,Transactions American GeophysicalUnion,82(6):65.
Didier J and Barbarin B.1991.Enclaves and Granite Petrology.Elsevier,625.
Ernst WG.2005.Alpine and Pacific styles of Phanerozoic mountainbuilding:subduction-zone petrogenesis of continental crust.Terra Nova,17:165~188.
Fernando B,Pilar Mand Tatiana Z.2003.The Nature,Origin,andThermal Influence of the Granite Source Layer of CentralIberia.The Journal of Geology,111:579~595.
Gao Shan,Rudnick R L,Yuan Hongling,Liu Xiaoming,LiuYongsheng,Xu Wenliang,Ling Wenli,Ayers J,WangXuanche,Wang Qinghai.2004.Recycling lower continentalcrust in the North China craton.Nature,432:892~897.
Geisler T,Ulonska M,Schleicher H,Pidgeon R T,Bronswijk WV.2001a.Recrystallization of metamorphic zircon underexperi mental hydrothermal conditions.Contrb.Petrol.,141:53~65.
Griffin W L,Zhang A D,O’Reilly S Y,Ryan C G.1998.Phanerozoic evolution of the lithosphere beneath the Sino-Korean Craton.In:Flower MFJ,Chung S L,Lo C Hand LeeT Y.eds.Mantle Dynamics and Plate Interactions in EastAsia.AGU Geodynamics Series,27:107~126.
Hanns P L,CIark I,Uwe A,Roland O.2002.Behavior of zirconduring high-pressure,low-temperature metamorphism:Casestudy fromthe Internal Unit of the Sesia Zone(Western Italian Alps).Eur.J.Mineral,14:61~71.
Hart mann L A,Leite J A D,Silva L C,Remus M V D,McNaughton N J,Groves D I,Fletcher I R,Santos J O S,Vasconcellos M A Z.2000.Advances in SHRI MPgeochronology and their i mpact on understanding the tectonicand metallogenic evolution of southern Brazil.AustralianJournal of Earth Sciences,47:829~844.
He Bin,Xu Yigang,Long Xiao,Wang Kai min,Sha Shaoli.2003.Generation and Spatial Distribution of the Emeishan LargeIgneous Province:New Evidence from Stratigraphic Records,77(2):194~202.
Hinton R W and Upton B G J.1999.The chemistry of zircon;variations within and between large crystals from syenite andalkali basalt xenolith.Geochi m.Cosmochi m.Acta,55:3287~3302.
oskin P WOand Black L P.2000b.Metamorphic zirconformationby solid-state recrystallization of protolith igneous zircon.J.metamorphic Geol.,18:423~439.
Huppert H E and Sparks R S J.1988.The generation of graniticmagmas by intrusion of basalt into continental crust.J.Petrol.,29:599~624.
Johannes W.1996.Petrogensis and Experi mental Petrology ofGranitic Rocks.Berlin:Spring-verlag,335.
Johmston A D and Wyllie P J.1998.Constraints on the origin ofArchean trondhjemites based on phase relationships of Nukgneiss with H2Oat15kbar.Contrib.Petrol.,100:35~46.
Keay S,Steele Dand Compston C.1999.Identifying granite sourcesby SHRI MP U-Pb zircon geochronology:an application to theLachlan foldbelt.Contrib Mineral Petrol,137:323~341.
Kinny P D,Strachan R A,Kocks H,Friend C R L.2003.U-Pbgeochronology of late Neoproterozoic augen granites in theMoine Supergroup,NWScotland:dating of rift-related,felsicmagmatism during supercontinent break-up-London:Journalof the Geological Society,160:925~934.
Klotzli U S,Koller F,Scharbert S,Hock V.2001.Variscangranite petrogenesis:Constraints from zircon typology andgeochronology,whole-rock and feldspar Pb—Sr isotopesystematics.Journal of Petrology,42:1621~1642.
Lo Ching-Hua,Chung S L,Lee T Yand Wu Genyao.2002.Age ofthe Emeishan flood magmatism and relations to Permian—Triassic boundary events.Earth Planet.Sci.Lett,198:449~458.
Leo A H and Jodo O S.2003.Predominance of high Th/U,magmatic zircon in Brazilian Shield sandstones.Geology,32:73~76.
Mc Menamin M A S,Mc Menamin D L S,1990.The Emergence ofAni mals:The Cambrian Breakthrough.New York:ColumbiaUniversity Press,1~12.
Martin J W and John P P.2003.Dating high-grademetamorphism——constraints from rare-earth elements inzircon and garnet.Contrb.Petrol.,145:61~74.
Menzies M A,Fan Wei ming,Zhang Ming.1993.Palaeozoic andCenozoic lithoprobes and the loss of>120km of Archaeanlithosphere,Sino-Korean craton,China.In:Prichard H M,Alabaster T,Harris N B W,Neary C R.eds.MagmaticProcesses and Plate Tectonics.Geol Soc Spec Publ,76:71~81.
Mezger K,Krogstad E J.1977.Interpretation of discordant U-Pbzircon ages——an evalution.Metamorph Geol.,15:127~140.
Pablo S,Herve M,Claude R,Michel M.2002.Transition fromcala-alkalic to adakitic magmatism at Cayambe volcanoEcuador:Insights into slab melts and mantle wedgeinteractions.Geology,30(11):967~970.
Patino Douce A Eand Beard J S.1996.Effects ofP,f2and Mg/Feratio on dehydration melting of model metagreywackes.J.Petrol,37:999~1024.
Patino Douce A Eand McCarthy TC.1998.Melting of crustal rocksduring continental collision and subduction.In:HackerB R,Liou J G.Eds,When Continents Collide:Geodynamics andGeochemistry of Ultrahigh-Pressure Rocks.Petrology andStructural Geology,Vol.10.Dordrecht:Kluwer AcademicPublishers,27~55.
Petford N,Paterson B,McCaffrey,Pugliese S.1996,Meltinfiltration and advection in microdioritic enclaves.Eur.J.Mineral,8:405~412.
Pidgeon R T,Nemchin A A and Hitchen G J.1998.Internalstructures of zircons from Archaean granites from the DarlingRange batholith:i mplications for zircon stability and theinterpretation of zircon U-Pb ages.Contributions to Mineralogyand Petrology,132:288~299.
Pitcher W S.1997.The Nature and Origin of Granite.London:Chapman and Hall Poli G,Tommasini S,Halliday A N.1996.Trace element and isotopic exchange during acid—basic magmainteraction processes.Trans.R Soc.Edinburgh:Earth Sci,87:225~232.
Poller U,Liebetrau V,Todt W.1997.U-Pb single-zircon datingunder cathodoluminescence control application topolymetamorphic orthogneisses.Chem Geol.,139:287~297.
Prouteau G,Scaillet B,Pichavant M,Maury R.2001.Evidence formantle metasomatism by hydrous silicic melts derived fromsubducted oceanic crust.Nature,410:197~200.
Pupin J P.1980.Zircon and granite petrology.Contrib.Petrol.,73:207~220.
Rainer A,Albert H,Hegner E,Langer C,Kreuzer H.2000.High-potassium,calc-alkaline I-type plutonismin the Europeanvariscides:northern Vosges(France)and northernSchwarzwald(Germany).Lithos,50:51~73.
Rapp R P,Watson E B and Miller C F.1991.Partial melting ofamphibolite/eclogite and origin of Archean trondhjemites andtonalities.Precamb.Res.,51:1~25.
Rapp R P,Watson E B.1995.Dehydration melting of metabasalt at8~32kbar:i mplications for continental growth and crust—mantle recycling.I.Petrol,36:891~931.
Roberts M P and Clemens J D.1993.Origin of high-potassium,calc-alkaline,I-type granitoids.Geology,21:825~828.
Rogers J W and Greenberg J K.1990.Late-orogenic,post-orogenic,and anorogenic granites:distinction by major-element and trace-element chemistry and possible origins.TheJournal of Geology,98:291~309.
Vavra G,Schaltegger U.1999a.Post-granulite facies monazitegrowth and rejuvenation during Permian to Lower Jurassicthermal events in the Ivrea Zone(Southern Apls).Contrib.Petrol.,134:405~414.
Vavra G,Schmid R and Gebauer D.1999b.Internal morphology,habit and U—Th—Pb microanalysis of amphibolite to granulitefacies zircons:Geochronology of the Ivrea Zone(SouthernAlps).Contributions to Mineralogy and Petrology,134:380~404.
Viebe R A,Manon M R,Hawkins D P,Hawkins,Mcdonoufh W F.2004.Late-Stage Mafic Injection and Thermal Rejuvenationof the Vinalhaven Granite,Coastal Maine.Journal ofPetrology,45(11):2133~2153.
Von Blanckenburg F,Kagami H,Deutsch A,Oberli F.1998.Theorigin of Alpine plutons along the Periadriatic Lineament.Schweiz.Mineral.Petrogr.Mitt,78:55~66.
Winther K T and Newton R C.1991.Experi mental melting ofhydrous low-K tholeiite:evidence on the origin of Archeancratons Bull.Geol.Soc.Den,39:213~228.
Wolf MBand Wyllie J P.1994.Dehydration-melting of amphiboliteat10kbar:the effects of temperature and ti me.Contrib.Petrol,115:369~383.
Wu Cailai,Wooden J L.,Yang Jingsui,Robinson P T,ZhengLingsen,Shi Rendeng and Chen Songyong.2006.Graniticmagmatismin the North Qaidam Early Paleozoic Ultra high-Pressure Metamorphic Belt,Northwest China.InternationalGeology Review,48:223~240.
Xia Linqi,Xia Zuchun and Xu Xueyi.2003.Magmagenesis in thOrdovician backarc basins of the North Qilian MountainChina.Geological Society of America Bulletin,115:1510~1522.
Xu Yigang,Chung S L,Jahn B,Wu Genyao.2001.Petrologic andgeochemical constraints on the petrogenesis of Permian—Triassic Emeishan flood basalts in southwestern China.Lithos,58:145~168.
Xu Yigang,Huang Xiaolong,Ma Jinlong,Wang Yanbin,Yoshiyuki Iizuka,Xu Jifeng,Wang Qiang,Wu Xiangyang-.2004.Crust—mantle interaction during the tectonic—thermalreactivation of the North China Craton:constraints fromSHRI MP zircon U-Pb chronology and geochemistry of Mesozoicplutons from western Shandong.Contrib.Petrol.,147:750~767.
Zhang Hongfu,Sun Min,Zhou Xinhua,Fan Wei ming,ZhaiMingguo,Yin Jifeng.2002.Mesozoic lithosphere destructionbeneath the North China Craton:evidence from major-,trace-element and Sr—Nd—Pbisotope studies of Fangcheng basalts.Contrib.Petrol.,144:241~253.
Zhang Hongfu,Sun Min,Zhou Xinhua,Zhou Meifu,Fan Wei ming,Zheng Jianping.2003.Secular evolution of the lithospherebeneath the eastern North China Craton:evidencefromMesozoic basalts and high-Mg andesites.Geochi mCosmochi m Acta,67:4373~4387.
Zhang Hongfu,Sun Min,Zhou Meifu,Fan Wei ming,Zhou Xinhua,Zhai Mingguo.2004.Highly heterogeneous late Mesozoiclithospheric mantle beneath the north China Craton:evidencefromSr—Nd—Pb isotopic systematics of mafic igneous rocks.Geol Mag,141(1):55~62.
Zhou Meifu,Malpas J,Song Xieyan,Robinson P T,Sun Min,Kennedy A K,Lesher C M,Keays R R.2002.Atemporal linkbetween the Emeishan large igneous province(SW China)andthe end-Guadalupian mass extinction.Earth and PlanetaryScience Letters,196:113~122.