中国东部燕山期和四川期岩石圈构造滑脱与岩浆起源深度
|
摘要
较确切地研究岩石圈内部构造滑脱面在地质历史时期形成的时间和部位是当前大地构造学研究的一个重要课题。通过大量收集中国东部燕山期(205~135Ma)和四川期(135~52Ma)岩浆起源深度资料来判断岩石圈内部和底部是否存在局部的构造滑脱界面,是否发生层圈相互作用,是否发生部分的解耦现象,是一种可行的研究方法。研究表明,中国东部燕山期和四川期岩石圈板块的构造滑脱、圈层的解耦作用及相互作用主要集中在中地壳、莫霍面与区域性主干断层的交线附近,而岩石圈板块的底面却并不存在大幅度的滑移。中国东部燕山期和四川期岩浆活动比较发育的地区基本上都位于大兴安岭—山西西部—武陵山—十万大山一线以东地区,而在此线以西地区岩浆活动相当微弱。笔者认为,在侏罗—白垩纪时期,该线以西缺少岩浆活动的地区可能就是当时的大陆型岩石圈,而该线以东岩浆活动剧烈的地区可能就属于海陆过渡型岩石圈。中国东部岩石圈的转型和"变薄",不太可能是深部地幔羽、去根作用、深部地幔热物质上涌或大陆伸展作用的结果,也不太可能与太平洋板块的俯冲作用有直接联系。
It is an important project for present tectonics to precisely research the time and space of the detachment formation in the lithosphere in geological history.It is a feasible research method that through collecting a lot of data of magmatic source depths in Eastern China during the Yanshanian (205-135 Ma) and Sichuanian (135-52 Ma) tectonic stages to determine the local tectonic detachment, the partial decoupling and the interaction between spheres in the lithosphere or at the bottom of the lithosphere.The results showed that the tectonic detachment, the partial decoupling and the interaction between spheres were exhibited and concentrated at the intersection of the middle crust, the Moho and the regional main faults of Eastern China during Yanshanian and Sichuanian tectonic stages, however, at the bottom of the lithosphere does not exist obvious detachment or migration in those stages.The violent magmatic area of Eastern China during the Jurassic and Cretaceous mainly distributed to the east boundary of Da Hinggan Ling-western Shanxi-Wulingshan-Shiwandashan, and to the west of this boundary the magmatism was very weak.The authors propose that there was the continental type of lithosphere to the west of that boundary, and the oceanic-continental transition type of lithosphere (continental crust with oceanic lithospheric mantle) to the east of that boundary.The lithosphere transformation and thinning of Eastern China in the Jurassic probably resulted neither from the mantle plume, un-rooting, upsurge of heat mantle materials and continental rifting, nor directly from the subduction of the Pacific plate.
It is an important project for present tectonics to precisely research the time and space of the detachment formation in the lithosphere in geological history.It is a feasible research method that through collecting a lot of data of magmatic source depths in Eastern China during the Yanshanian (205-135 Ma) and Sichuanian (135-52 Ma) tectonic stages to determine the local tectonic detachment, the partial decoupling and the interaction between spheres in the lithosphere or at the bottom of the lithosphere.The results showed that the tectonic detachment, the partial decoupling and the interaction between spheres were exhibited and concentrated at the intersection of the middle crust, the Moho and the regional main faults of Eastern China during Yanshanian and Sichuanian tectonic stages, however, at the bottom of the lithosphere does not exist obvious detachment or migration in those stages.The violent magmatic area of Eastern China during the Jurassic and Cretaceous mainly distributed to the east boundary of Da Hinggan Ling-western Shanxi-Wulingshan-Shiwandashan, and to the west of this boundary the magmatism was very weak.The authors propose that there was the continental type of lithosphere to the west of that boundary, and the oceanic-continental transition type of lithosphere (continental crust with oceanic lithospheric mantle) to the east of that boundary.The lithosphere transformation and thinning of Eastern China in the Jurassic probably resulted neither from the mantle plume, un-rooting, upsurge of heat mantle materials and continental rifting, nor directly from the subduction of the Pacific plate.
引文
①江西地质科学研究所.江西省花岗岩类的基本特征及与钨矿成矿的关系.1983.
①江西地质科学研究所.江西省花岗岩类的基本特征及与钨矿成矿的关系.1983.
①江西地质科学研究所.江西省花岗岩类的基本特征及与钨矿成矿的关系.1983.
[1]Wan T F.An outline of tectonics of China[M].Beijing:Ge-ological Publishing House,2004:1-387(in Chinese).
[2]Teng J W,Zeng R S,Yan Y F.Depth distribution and basic framework of Moho discontinuity in Eastern Asian continent and adjacent sea areas[J].Science in China:Series D,2002,32(2):89-100(in Chinese).
[3]Liu G D.Geodynamical evolution and tectonic framework of China[J].Earth Science Frontiers,2007,14(3):39-46(in Chinese).
[4]Cai X L,Zhu J S,Cao J M,et al.Structure and dynamic of lithosphere and athenosphere of Eastern Asian-Western Pacif-ic giant rift system[J].Geologyin China,2002,29(3):234-245(in Chinese).
[5]Zhu J S.The structural characteristics of lithosphere in the continent of Eurasia and its marginal seas[J].Earth Science Frontiers,2007,14(3):1-20(in Chinese).
[6]Lu F X,Wu Q F.Composition,structure and spheres inter-action of lower lithosphereintypical areas of East China[M].Wuhan:China University of Geosciences Press,2005:1-195(in Chinese).
[7]Compile Group of Petroleum Geology.Daqing oil field[M]∥Zhai G M.Petroleumgeology,Vol.2(Ⅰ).Beijing:Petrole-umIndustry Press,1993:34-40(in Chinese).
[8]Wang K H,Pei F P,Feng YS,et al.Discovered deep source inclusion andinclusion crystal and their mineral-chemistry of Mesozoic volcanic rocks in Mingyuegou Basin,Yanbian[J].Jilin Geology,2005,24(2):21-27(in Chinese).
[9]Zhao Q G,Xu W L,Jin K,et al.Magmatic source area of Mesozoic volcanic rocks in Yanbian area:evidences form Sr-Ndisotope and deep sourceinclusion[J].Journal of Jilin Uni-versity:Earth Science Edition,2005,35(4):416-422(in Chinese).
[10]Sun D Y,Wu F Y,Lin Q,et al.Origin of Baishishanintru-sion and interaction between crust and mantle during Early Yashanianin Zhangguangcailing[J].Acta Petrologica Sinica,2001,17(2):227-235(in Chinese).
[11]Lin Q,Ge W C,Wu F Y,et al.Granitoid geochemistry of Mesozoic in Da Hinggan Ling[J].Acta Petrologica Sinica,2004,20(3):403-412(in Chinese).
[12]Yin Z G,Zhang Y L,Yang X P,et al.Characteristics and magmatic evolution of Mesozoic volcanic rocks at northern Da Hinggan Ling[J].Global Geology,2006,25(2):120-128(in Chinese).
[13]Xue G,Luo J Y,Liu J Y.Mesozoic volcanic rock character-istics and originin middle-southern Da Hinggan Ling[J].Sci-ence,Technology and Economy of Inner Mongolia,2006,4:100-102(in Chinese).
[14]Xiao C D,Zhang Z L,Zhao L Q.Nd,Sr,Pb isotope and rock origin of Yanshanian granite in eastern Inner Mongolia[J].Geology in China,2004,31(1):57-63(in Chinese).
[15]Chen Y X,Chen WJ,Zhou X H,et al.Mesozoic volcanic rock in western Liaoning and adjacent area[M].Beijing:Seismological Press,1997(in Chinese).
[16]Shao J A,Zhai M G,Zhang L Q,et al.Determined dyke swarminfive stages andits tectonic significance at the margin among Shanxi,Hebei andInner Mongolia[J].Acta Geologica Sinica,2005,79(1):56-67(in Chinese).
[17]Hong D W,Wang T,Tong Y.Mesozoic granitoids from North China block and Qinling-Dabie-Sulu orogenic belt and their deep dynamic process[J].Earth Science Frontiers,2003,10(3):231-256(in Chinese).
[18]Yan G H,Xu B L,Mu B L,et al.Alkaline intrusion at the east foot of the Taihang-Da Hinggan Ling:choronology,Sr,Nd and Pbisotopic characteristics and their i mplications[J].Acta Geologica Sinica,2000,74(4):774-781(in Chinese).
[19]Wei J H,Liu C Q,Tang H F.Trace element,isotopic evi-dence in syn-original magmatismof Yanshanianintrusions and gold mineralization at Wulong area of Liaoning[J].Geological Review,2003,49(3):265-271(in Chinese).
[20]Zhang Q,Zhao T P,Wang Y,et al.Some problems of mag-matismin Yanshanian of eastern China[J].Journal of Petrol-ogy and Mineralogy,2001,20(3):273-280,292(in Chi-nese).
[21]Jiang Y H,Jiang S Y,Zhao K D,et al.SHRI MP zircon U-Pb age of lamprophyre at East Liaoning Peninsula and restric-tion of beginningti me for lithosphere thinning of Eastern Chi-na[J].Chinese Science Bulletin,2005,50(19):2161-2168(in Chinese).
[22]Wang Y,Deng J F.Petrochemical characteristics and geody-namic significance of the Yanshanian strongly peraluminous intrusive rocks in the Hebei-Shanxi-Liaoning area[J].Geo-logical Bulletin of China,2002,21(4-5):270-276(in Chi-nese).
[23]Wu L R.Meso-Cenozoic volcanic rocksin East China and ad-jacent areas[M].Beijing:Science Press,1984(in Chinese).
[24]Chen Z H,Lu S N,Li H K,et al.Age of the Fushui inter-mediate-mafic intrusive complex in the Qinling orogen:new zircon U-Pb and whole-rock Smand Ndisotope chronological evidence[J].Geological Bulletin of China,2004,23(4):322-328(in Chinese).
[25]Zhang H,Yuan H L,Hu Z C,et al.Rare earth element characteristics andits significance of single zirconin Mesozoic volcanic rocks,in Luanping of Hebei[J].Journal of Rare Earth Element in China,2006,24(2):227-234(in Chinese).
[26]Xu WL,Lin J Q.The discovery and study of mantle-derived dunite inclusions in hornblende-diorite in the Handan-Xingtai area,Hebei[J].Acta Geologica Sinica,1991,65(1):33-41(in Chinese).
[27]Li WP,Li X H.Origin and its significance of Middle-Late Jurassic intermediate-acid volcanic rocks,in middle Yanshan orogenic zone[J].Acta Petrologica Sinica,2004,20(3):247-254(in Chinese).
[28]Niu S Y,Chen L,Xu C S,et al.The crustal evolution and metallogenic regularity of the Taihangshan Area[M].Bei-jing:Seismological Press,1994:1-203(in Chinese).
[29]Wan T F,Teyssier C,Zeng HL,et al.Emplacement mech-anism of Linglong granitoid complex,Shandong Peninsula,China[J].Science in China:Series D,2001,44(6):535-544(in Chinese).
[30]Luo Z K,Miao L C.Granites and gold depositsin Zhaoyuan-Laizhou Area,Eastern Shandong Province[M].Beijing:Metallurgical Industry Press,2002:20-57(in Chinese).
[31]Guo J H,Chen F K,Zhang X M,et al.Mesozoic magmatic intrusion and syn-collision-post-collision tectonicsin Northern Sulu UHP belt,eastern China:SHRI MP zircon U-Pb geo-chronology[J].Acta Petrologica Sinica,2005,21(4):1281-1301(in Chinese).
[32]Sun F Y.Mesozoic-Cenozoic regional tectonic evolution and mineralizationin Eastern Shandong[J].Journal of Changchun Institute of Geology,1994,24(4):378-384(in Chinese).
[33]Chen G Y,Sun D S,Zhou X R,et al.Genetic mineralogy and gold mineralization of Guojialing granodiorite in Jiaodong region[M].Wuhan:China University of Geosciences Press,1993:1-230(in Chinese).
[34]Compile Group of Petroleum Geology.Shengli oil field[M]∥Zhai G M.Petroleum geology,Vol.6.Beijing:Petroleum Industry Press,1993:264-271(in Chinese).
[35]Zeng J N,Zuo D H,Ma X.Yanshanian magmatic evolution andits influence to metal mineralizationin Ta ershan,Shanxi[J].Journal of Geology and Mineral Resources of North Chi-na,1997,12(1):33-43(in Chinese).
[36]Zhen Y Q.Isotopic geochemistry andits mineralization model of gold,silver,multi-metal ore depositsin Wutaishan-Hengs-han[J].Journal of Technology Institute of Guilin,2004,24(2):127-136(in Chinese).
[37]Shanxi Bureau of Geology and Mineral Resources(Shanxi Ge-ological Survey).Regional geology of Shanxi Province[M].Beijing:Geological Publishing House,1989:1-780(in Chi-nese).
[38]Li S G,Huang F,Li H.Post collision lithosphere detach-ment in Dabie-Sulu orogenic belt[J].Chinese Science Bulle-tin,2001,46(17):1487-1491(in Chinese).
[39]Guan Y C,Wu H Q.Characteristics of Bai majian ultra-unite and its origin[J].Anhui Geology,1997,7(2):26-35(in Chi-nese).
[40]Depart ment of Geology,Nanjing University.South China granitoids and their mineralizations[M].Beijing:Science Press,1981(in Chinese).
[41]Du Y S,Qin X L,Li XJ.Mesozoic mantle source magmatic underplating of Tongling,Anhui—evidences fromgreat crys-tal and rockinclusion[J].Journal of Petrology and Mineralo-gy,2004,23(2):109-116(in Chinese).
[42]Wang Y L,Wang X,Zhang Q.The geochemical characteris-tics of Mesozoic intermediate-acid intrusives of the Tongling area andits metallogenesis-geodynamic i mplications[J].Acta Petrologica Sinica,2004,20(2):325-338(in Chinese).
[43]Lou Y E,Du Y S.Characteristics and original discussion of biotite in Mesozoic intrusion of Fanchang-Tongling,Anhui[J].Journal of Mineralogy,2006,26(2):175-180(in Chi-nese).
[44]Wang Y B,Liu D Y,Zeng P S,et al.Underplating choron-ology of mantle magmain Tongling,Anhui—zircon SHRI MP dating in Chaoshan pyroxene diorite[J].Acta Geoscientica Sinica,2004,25(4):423-427(in Chinese).
[45]Xu WL,Wang Q H,Wang D Y,et al.Mesozoiclithosphere thinning and mechanismof eastern North China Craton:evi-dences of deep inclusion of Mesozoic magmatic rocks[J].Earth Science Frontiers,2004,11(3):309-317(in Chinese).
[46]Zhai Y S,Yao S Z,Zhou X R,et al.Metallogeny of iron,copper and goldin Lower and Middle Reaches of Yangtze Riv-er[M].Beijing:Geological Publishing House,1992:1-235(in Chinese).
[47]Zhou T X,Chen J F,Li X M,et al.Query the Indosinian magmatismin Anhui[J].Acta Petrologica Sinica,1988(3):46-53(in Chinese).
[48]Wang D Z,Zhou X M,Shu L S,et al.Origin of granitic vol-canic-intrusion complex and crustal evolution during Late Mesozoic in Southeast China[M].Beijing:Science Press,2002(in Chinese).
[49]Li YJ,Xie QS,Luan X D,et al.Origin andtectonic signifi-cance of West Qinling Michuling magma belt[J].Xinjiang Geology,2004,22(4):374-377(in Chinese).
[50]Liu A P,Jin J F.Research on zircon typomorphic character-istics in Muhuguan granite[J].Geology and Geochemistry,1996,4:15-20(in Chinese).
[51]Shang RJ,Yan Z,Huang Y Y,et al.Granitein Qinling and Dabashan[M].Wuhan:China University of Geosciences Press,1988(in Chinese).
[52]Hu HZ,Li Y.Restrict factor of Yanshanian magmatismto gold and silver mineralization in Xiong ershan,western Henan[J].Mineralization and Geology,2006,20(4-5):427-429(in Chinese).
[53]Yan Z,Xu Q C,Zhang HJ,et al.Granite in Shaanxi Prov-ince[M].Xi an:Xi an Communication University Press,1985(in Chinese).
[54]Yang Q,Wu C L,Tang D Z,et al.Coal metamorphismin China[M].Beijing:Coal Industry Press,1996:1-212(in Chinese).
[55]Zhu J S,Cai X L,Cao J M,et al.The three-di mensional structure of lithosphere and its evolution in South China and East China Sea[M].Beijing:Geological Publishing House,2005:1-308(in Chinese).
[56]Gao TJ,Wang Z M,Wu K L,et al.Tectono-magmatic evo-lution and metallogeny of Tai wan Strait andits adjacent areas[M].Beijing:Geological Publishing House,1999:1-203(in Chinese).
[57]Li X Q,Chen J D,Pan MB,et al.Petrological suits of Mes-ozoic intrusionin Chengtou area,Ganyu,Jiangsu[J].Jiangsu Geology,1999(2):80-83(in Chinese).
[58]Zhou X R,Yang J,Ren J.Comparative study on the charac-teristics and genesis between I-and A-type granite of Suzhou area[J].Earth Science,1997,22(3):240-246(in Chinese).
[59]Zhou T F,Yuan F,Hou MJ,et al.Origin of Yanshanian granite and geodynamic background in the boundary between Anhui and Jiangxi of Jiangnan Uplift area[J].Journal of Mineralogy and Petrology,2004,24(3):65-71(in Chinese).
[60]Jiang G H,Hu R Z,Xie G Q,et al.Biotite geochemistry characteristics and influences of rock and ore deposit forma-tionin Dajishan granite[J].Journal Mineralogy and Petrolo-gy,2005,25(5):58-61(in Chinese).
[61]Chen P R,Hua R M,Zhang B T,et al.Early Yanshanian post-orogenic granitoids in the Nanling region:petrological constraints and geodynamic settings[J].Science in China:Series D,2002,45(8):755-768(in Chinese).
[62]Li X H,Chen Z G,Liu D Y,et al.Jurassic gabbro-granite-syenite suites fromsouthern Jiangxi Province,SE China:age,origin and tectonic significance[J].International Geological Review,2003,45:898-921.
[63]Chen X M,Lu J J,Liu C S,et al.Single zircon U-Pb age in Tonglu-Xiangshan volcanic-intrusion complex[J].Acta Pet-rologica Sinica,1999,15(2):272-278(in Chinese).
[64]Ling HF,Shen WC,Huang X L.Nd-Sr isotopic character-istics of granitoid and their significances in Fujian[J].Acta Petrologica Sinica,1999,15(2):255-262(in Chinese).
[65]Luo X H.Mesozoic magmatismandits tectonic significancein Jiujiang-Ruichang areas[J].Journal of Institute of Technolo-gy of East China,2006,29(2):121-126(in Chinese).
[66]Yu X Q,Su L S,Deng G H,et al.Geochemistry character-istics andits tectonic significance of alkali basalt in Jitai Ba-sin,Jiangxi[J].Geoscience,2005,19:133-140(in Chi-nese).
[67]Lai Z Z,Wang A C.Mesozoic volcanic activity age and mag-matic sourcein South Jiangxi[J].Jiangxi Geology,1996,10:111-118(in Chinese).
[68]Zhou J C,Jiang S Y,Wang X L,et al.Petrological-geo-chemistry for Middle Jurassicin South China—example to ba-salt of Fankeng in Fujian[J].Science in China:Series D,2005,35(10):927-936(in Chinese).
[69]Jiang J L.Two distinguish macro-volcanic zones of Late Ju-rassic in Fujian[J].Fujian Geology,2001,20(4):171-176(in Chinese).
[70]Zhang WL,Hua R M,Wang R C,et al.Research onforma-tion of granite andforming age of Tungsten ore deposit at Da-jishan,South Jiangxi[J].Acta Geologica Sinica,2006,80(7):956-962(in Chinese).
[71]Wu G Y.Chronology of Guangning granite complex[J].Guangdong Geology,1986,1:1-22(in Chinese).
[72]Ye B D.Isotopic ages andits geological significancein Yunkai area of Guangdong and Guangxi[J].Guangdong Geology,1989,3:39-55(in Chinese).
[73]Cui Y.Isotopic chronology and origin evolution of Hetai granite[C]∥Proceedings of4th China Isotopic Conference,1989:58-59(in Chinese).
[74]Wang L K,Sha L F,Xu WX,et al.Discussion onformation and series of granite—also discussion on three original divi-sions[M].Guangzhou:Guangdong Science and Technology Press,2003(in Chinese).
[75]Geng HY,Xu XS,O Reilly S Y,et al.Cretaceous volcanic-intrusionin western Guangdong andits geological significance[J].Science in China:Series D,2006,36(7):601-617(in Chinese).
[76]Hua R M.Differential ti me between continental crust remelt granite and mineralization,and their geological influence[J].Geological Review,2005,51(6):27-33(in Chinese).
[77]Zhang S M,Wu J H,Zhou WX,et al.Nd-Sr isotopic study for mafic rocks of Yanshanian at eastern Nanling[J].Journal of Institute of Technology of East China,2004,27(2):129-135(in Chinese).
[78]Ma T Q,Kuang J,Bo D Y,et al.Granite geochemistry characteristics and their analysis of formation tectono-envi-ronment at south Zhuguangshan of Middle Nanling[J].Geolo-gy in China,2006,33(1):119-131(in Chinese).
[79]Chen P R,Zhou X M,Zhang WL,et al.Origin and influ-ence of syenite-granite complex of Early Yanshanian at east-ern part of Nanling[J].Science in China:Series D,2004,34(6):493-503(in Chinese).
[80]Gilder S A,Gill J B,Coe R S,et al.Isotopic and paleomag-netic constraints on the Mesozoic tectonic evolution of South China[J].J Geophys Res,1996,101(B7):16137-16155.
[81]Fu J M,Ma C Q,Xie C F,et al.Determined Atype of alumi-nous granite and tectonic environment analysis in Jinjiling of Hu-nan[J].Geochemistry,2005,34(3):215-226(in Chinese).
[82]Li X H,Chung S L,Zhou H W,et al.Jurassic intraplate magmatismin southern Hunan-eastern Guangxi:40Ar/39Ar dating,geochemistry,Sr-Ndisotopes andi mplications for tec-tonic evolution of SE China[M]∥Malpas J,Fletcher C J,Ai-tchison J C,et al.Aspects of the tectonic evolution of China.Geological Society,London,Special Publications,2004,226:193-216.
[83]Kong H,Ma F,Huang D Z.Deep rock sectionin Hunan ar-ea:evidence fromdeep sourceinclusions[J].Journal of Insti-tute of Technology of Guilin,2001,21(3):195-201(in Chi-nese).
[84]Chen B H,Jia B H,Liu Y R,et al.Sm-Nd isochron age of spinel lherzolite inclusionin Mesozoic volcanic rocks of South Hunan[J].Geological Review,2004(2):180-183(in Chi-nese).
[85]Gu C Y,Hua R M,Qi H W.Single zircon LA-ICP-MS U-Pb dating and whole rock Sr-Nd isotopic of Guposhan granite in Guangxi[J].Acta Geologica Sinica,2006,80(4):543-553(in Chinese).
[86]Guo X S,Chen J F,Zhang X,et al.Ndisotopic composition of alkali magmatic complexin southeast Guangxi:South Chi-na Mesozoic mantle material uplift event[J].Acta Petrologica Sinica,2001,17(1):19-27(in Chinese).
[87]Wang J H,Jiang B C,Kong X W,et al.Basic characteristics of Guposhan complexintrusion and relationship with mineral-ization[J].Mineralization and Geology,2006,20(1):47-53(in Chinese).
[88]Zeng H L,Liu J,Zhang Q H.Gravity and magnetic data processing and interpretation and its application to research on crustal structure,South China[M]∥1994Annual Report,Laboratory of Lithosphere Tectonics and Dynamics.Beijing:Seismological Press,1995:87-101(in Chinese).
[89]Zhan M G.Tectonic-magmatism-mineralization and regional metallogenic research of Mesozoic in South China[D].Yichang:Yichang Institute of Geology and Mineral Re-sources,CAGS,1994(in Chinese).
[90]Chen X,Xiao L.Geochemistry research on Erentaolegai sil-ver ore deposit,Inner Mongolia[J].Precious Metal Geology,1999,8(3):171-178(in Chinese).
[91]Shao J A,Jia W,Chu Z Y,et al.Early Cretaceous olivine-pyroxene minette volcanic pipe in Karaxin,Inner Mongolia[J].Acta Petrologica Sinica,2003,19(3):429-434(in Chi-nese).
[92]Zhang H F,Zheng J P.Geochemistry characteristics and rock origin for Mesozoic basalt in North China—case of Fux-in,Liaoning[J].Chinese Science Bulletin,2003,48(6):603-609(in Chinese).
[93]Lu F X,Zhu Q W,Li S T,et al.Mesozoic volcanismsur-rounding Songliao basin,China:i mplication for the relation-ship with evolution of basin[J].Journal of China University of Geosciences,1997,8(1):72-77.
[94]Lu F X,Zhu Q W,Xie Y H,et al.Discovery of giant crystal of high pressure pyroxene in dacite and its significance[J].Earth Science—Journal of China University of Geosciences,1996,21(5):541-544(in Chinese).
[95]Zhang H H,Xu Y G,Ge W C,et al.Basalt geochemistry characteristic andits significance during Late Mesozoic-Ceno-zoic in Yitong-Datun areas,Jilin[J].Acta Petrologica Sinica,2006,22(6):1579-1596(in Chinese).
[96]Liu R X,Chen WJ,Xie G H,et al.Chronology and geo-chemistry of Cenozoic volcanic rocks in China[M].Beijing:Seismological Press,1992(in Chinese).
[97]Zhang X.Geological characteristics of Early Cretaceous rhyo-lite in Shanmen,Siping,Jilin[J].Jilin Geology,2001,20(3):30-34(in Chinese).
[98]Zheng C Q,Xu WL,Wang D Y.The petrology and mineral chemistry of deep-seated xenolithsin Mesozoic basalt in Fuxin district from western Liaoning[J].Acta Petrologica Sinica,1999,15(4):616-622(in Chinese).
[99]Shao J A,Li Z T,Zhang L Q.Ti me and space symmetry dis-tribution and significance of Mesozoic-Cenozoic volcanic rocks in western Liaoning and its adjacent areas[J].Scientia Geo-logica Sinica,2004,39(1):98-106(in Chinese).
[100]Zhang Z C,Li Z N,Wang F B,et al.Basic characteristic of volcanic rock andits origin in Yixian Basin,western Liaon-ing[J].Geoscience,1994,8(4):441-451(in Chinese).
[101]Shao J A,Zhang L Q,Wei CJ,et al.The composition and its characteristics of bi modal dyke swarm of Mesozoic at Nankou,Beijing[J].Acta Geologica Sinica,2001,75(2):205-212(in Chinese).
[102]Su S G,Deng J F,Zhao G C.Characteristics,origin,source region and thinning type of lithosphere Xuejiashiliang complex[J].Earth Science Frontiers,2006,13(2):148-157(in Chinese).
[103]Cai J H,Yan G H,Mu B L,et al.Zircon U-Pb age,Sr-Nd-Pbisotopic,trace elements and discussion on its origin[J].Acta Petrologica Sinica,2005,21(3):776-788(in Chi-nese).
[104]Shao J A,Li X H,Zhang L Q,et al.Geochemical condition for genetic mechanismof the Mesozoic bi modal dike swarms in Nankou-Guyaju[J].Geochi mica,2001,30(6):517-524(in Chinese).
[105]Compile Group of Petroleum Geology.Dagang oil field[M]∥Zhai G M.Petroleumgeology,Vol.4.Beijing:Petroleum Industry Press,1991:92-95(in Chinese).
[106]Chen B,Liu C Q,Tian W.Crust-mantle magma migmatiti-zation during Mesozoic in Taihangshan:evidences of petrol-ogy and geochemistry[J].Earth Science Frontiers,2006,13(2):140-147(in Chinese).
[107]Zhang Y,Chen B,Shao J A,et al.Geochemistry character-istics and discussion on origin for Late Mesozoic lampro-phyre in Taihangshan,North China[J].Journal of Mineral-ogy and Petrology,2003,22(1):29-33(in Chinese).
[108]Meng F C,Li T F,Xue H M,et al.Contrast withtwo Late Cretaceous basic magma(Zhucheng and Jiaozhou basalts,in Jiaolai Basin)formed in different mantle sources[J].Acta Petrologica Sinica,2006,22(6):1644-1656(in Chinese).
[109]Yan J,Chen J F,Xie Z,et al.Research on petrology and geochemistry of Late Cretaceous basalt and mantle inclusion in East Shandong[J].Acta Petrologica Sinica,2005,21(1):99-110(in Chinese).
[110]Zhang H F,Sun M.Geochemistry of Mesozoic basalts and mafic dikes,southeastern north china craton and tectonic i mplications[J].International Geological Review,2002,44:370-382.
[111]Zhang HF,Sun M,Zhou X H,et al.Secular evolution of the lithosphere beneaththe eastern North China Craton:ev-idence from Mesozoic basalts and high-Mg andesites[J].Geochi mica et Cosmochi mica Acta,2003,67(22):4373-4387.
[112]Yan J,Chen J F,Xie Z,et al.Mantle source inclusion of Late Cretaceous basalt in East Shandong:new evidence for ti me restrain of Eastern China lithosphere thinning[J].Chi-nese Science Bulletin,2003,48(14):1570-1574(in Chi-nese).
[113]Liu X H,Wang J R,Sun X L,et al.Research on granite and gold mineralization in Zhaoyuan-Yexian ore fields[J].Nonferrous Metal,2006,58(4):15-20(in Chinese).
[114]Pei F P.Mesozoic basalt and mineral-chemistry of crystal inclusion of mantle source:restrict to character of litho-sphere mantle[J].Journal of Geology of Universities,2004,10(1):88-97(in Chinese).
[115]Wang D Y,Xu WL,Lan X,et al.Origin of pyroxenite in-clusionin Mesozoic gabbro-diorite of Western Shandong[J].Journal of Jilin University:Earth Science Edition,2004,34(2):167-173(in Chinese).
[116]Wan T F.Tectonic evolution and stress fields of Shandong Province[J].Geology of Shandong,1992,8(2):70-101(in Chinese).
[117]Li X Y,Fan L Y.Discovery and its significance of Late Mesozoic OIBtype basalt in Western Qinling[J].Journal of Zhongshan University:Natural Science Edition,2006,45(3):127-128(in Chinese).
[118]Li J Z,Zhang A M.Original type and magmatic evolution characteristics of Mesozoic granite in Jinzhai-Suxian area of Northern Huaiyang[J].Geoscience,1997,11(2):253-260(in Chinese).
[119]Li S G,Huang F,Li H.Post-collision lithosphere detach-ment in Dabie-Sulu orogenic belt[J].Chinese Science Bulle-tin,2001,46(17):1487-1491(in Chinese).
[120]Wang Q,Zhao Z H,Jian P,et al.Chronology of Creta-ceous Atype granitoid or alkali intrusion in inland of South China and restrain for Late Mesozoic tectonic evolution in South China[J].Acta Petrologica Sinica,2005,21(3):795-808(in Chinese).
[121]Ma C Q,Yang K G,Xu C H,et al.Mesozoic Alkali mag-matism in Dabieshan and uplift mechanism of ultra-high pressure metamorphic block[J].Acta Petrologica Sinica,1999,15(3):379-395(in Chinese).
[122]Zhai J P.Sr isotopic characteristics and origin research of Kunshan,Chengshan and Dalongshan intrusions[J].Geo-chemistry,1989,3:202-209(in Chinese).
[123]Zhang D Q,Xu H L.Compare research on geology-geo-chemistry of granitoid in lower and middle reaches of Yan-gtze River[J].South China Geology and Resources,2002,3:66-77(in Chinese).
[124]Xing F M,Xu X.Two Atype granite zones in Anhui[J].Acta Petrologica Sinica,1994,10(4):357-369.
[125]Xing F M.Basic characteristics of Mesozoic magma along Yangtze River in Anhui[J].Acta Petrologica Sinica,1995,11(4):409-422.
[126]Li W D,Mao J R,Zhu Y H,et al.Mesozoic magmatism and ore deposits of Southeast China[M].Beijing:Seismo-logical Press,1998(in Chinese).
[127]Xing F M,Xu X.Magma rock zone and mineralization in Yangtze of Anhui[M].Hefei:People Publishing House of Anhui,1999:1-170(in Chinese).
[128]Jin K,Xu W L,Wang Q H,et al.Formation ti me and source area of grano-diorite in Huaiguang,Benfu:zircon SHRI MP U-Pb chronology evidence[J].Acta Geoscientica Sinica,2003,24(4):331-335(in Chinese).
[129]Yang D B,Xu WL,Pei F P,et al.Granite formation age and feature of magma source area for Benfu area:zircon LA-ICPMS U-Pb age dating and tracing[J].Geochemistry,2005,34(5):443-454(in Chinese).
[130]Niu ML.Compare research on rare earth elements of Early Cretaceous volcanic rockin south margin of Zhangbaling up-lift area[J].Journal of Rare Earth Element in China,2006,24(6):739-744(in Chinese).
[131]Wu C L,Zhou X R,Huang X C,et al.Research on Atype granite in Maotan,Anhui[J].Acta Geologica Sinica,1998,72(3):237-247(in Chinese).
[132]Zhang B T,Zhang F S,Ni QS,et al.Discussion on geolo-gy and geochemistry characteristics and originin quartz sye-nite zone of Anqing-Lujiang area[J].Acta Petrologica Sini-ca,1988,4(3):1-12(in Chinese).
[133]Yan J,Chen J F,Xie Z,et al.Geochemistry research of Late Mesozoic basalt in Kedoushan,lower and middle rea-ches of Yangtze River:mantle feature of lithosphere and e-volution restrain[J].Geochemistry,2005,34(5):455-469(in Chinese).
[134]Qi X X,Kuang H W,Chen P L,et al.Geochemistry char-acteristics and its geological significance of Yanshanian in-trusion in lower and middle reaches of Yangtze River[J].Resource Survey and Environment,2002,23(1):52-59(in Chinese).
[135]Xu W L,Wang Q H,Liu X C,et al.Chronology and sources of Mesozoic intrusive complex in Xu-Huai region,central China:constraints fromSHRI MPzircon U-Pb dating[J].Acta Geologica Sinica,2004,78(1):96-106.
[136]Chen J F,Foland K A,Liu Y M.Actural40Ar/39Ar age dating of granite complex in Suzhou[J].Acta Petrologica Sinica,1993,9(1):77-85(in Chinese).
[137]Ye S Q.Rb-Sr isochron age of Funiushanintrusionin Nan-jing-Zhenjiang,Jiangsu[J].Jiangsu Geology,1999,23(3):148-150(in Chinese).
[138]Gong X F,Guan J Q.Volcanic geological characteristics and evolutioninlower and middle reaches of Nanxijiang,South-east Zhejiang[J].Zhejiang Geology,1998,14(1):11-17(in Chinese).
[139]Chen J F.Explanation of isotopic data of si mple-mixed,AFC migmatite granite[J].Anhui Geology,1991,1:19-27(in Chinese).
[140]Wang Z J,Rang Q F,Ruan H H,et al.Some basic prob-lems of Mesozoic volcanic geologyin Zhejiang-Fujian-Jiangxi[J].Journal of Nanjing Institute of Geology and Resources,1987,8(3):1-14(in Chinese).
[141]Qiu J S,Wang D Z,McInnes BI A.Geochemistry and ori-gin of I and Atypes granite complex in coastal of Zhejiang and Fujian[J].Acta Petrologica Sinica,1999,15(2):237-246(in Chinese).
[142]Hong D W,Xie X L,Zhang J S.The geological significance of highεNdvalue granitic zone for Hangzhou-Zhuguangshan-Huashan[J].Geological Bulletin of China,2002,21(6):348-354(in Chinese).
[143]Zhou J C,Zhang HJ,Yu Y W.Magma migmatization in complex flowof Early Cretaceousin Xinchang,Zhejiang[J].Acta Petrologica Sinica,1994,10(3):236-247(in Chi-nese).
[144]Huang Q Z.Explanation of regional geological map of Fu-jian Province(1∶500000)[M].Fuzhou:Catastrophy Pub-lishing House of Fujian,1998:1-120(in Chinese).
[145]Qiu J S,Wang D Z,McInnes BI.Geochemistry and origin of aluminium Atype granite in coastal of Fujian[J].Geo-chemistry,2000,29(4):313-321(in Chinese).
[146]Qiu J S,Wang D Z,Zhou J C.Geochemistry and rock ori-gin of bi modal volcanic rocks during Late Mesozoic in Yun-shan,Yongtai,Fujian[J].Journal of Petrology and Miner-alogy,1999,18(2):97-107(in Chinese).
[147]Zhang D Q,She H Q,Yan K H,et al.Magmatic geochem-istry evidences for Mesozoic tectonic environments change at Zijinshan area of Fujian[J].Geological Review,2001,47(6):608-616(in Chinese).
[148]Hong D W,Guo W Q,Li GJ,et al.Miarolitic granite pe-trology and original evolution at coastal of Fujian[M].Bei-jing:Beijing Science and Technology Press,1987(in Chi-nese).
[149]Mao J R,Tao K Y,Li J Y,et al.Mesozoic grano-diorite characteristics andits tectonic evolutionin Southwest Fujian[J].Journal of Petrology and Mineralogy,2002,21(2):135-142(in Chinese).
[150]Zhou X R,Wu K L.I-Atype granite in Zhangzhou[M].Beijing:Science Press,1994(in Chinese).
[151]Liao Q A,Wang J M,Xue Z S,et al.Characteristics of two type basalts in Cretaceous basins of Guangfeng,Jiangxi and its relationship of basin evolution[J].Acta Petrologica Sini-ca,1999,15(1):116-123(in Chinese).
[152]Wang Y,Yu D G.Trace elements geochemistry characteris-tics and origin of intermediate-acid volcano-intrusion com-plex of Early Cretaceous in Northeast Jiangxi[J].Jiangxi Geology,2000,14(4):251-255(in Chinese).
[153]Yu X Q,Shu L S,Yan T Z,et al.Rock geochemistry and its tectonic significance of Early Cretaceous basalt in Jiangs-han-Guangfeng areas[J].Geochemistry,2004,33(5):465-474(in Chinese).
[154]Wang Z W,Zhou Y Z,Zhang H H,et al.Rare earth ele-ments geochemistry of silver deposit in Panxidong,western Guangdong[J].Gold Geology,1999,5(2):52-54(in Chi-nese).
[155]Zhang Z S.Basic characteristics and formation environment of Late Mesozoic alkali volcanic rock in Baiyuanzhang[J].Guangdong Geology,2001,16(4):22-28(in Chinese).
[156]Xu X S,Zhou X M,Reillysy O,et al.Lower crust material of Southeast China and discussion on origin[J].Acta Petro-logica Sinica,1999,15(2):217-223(in Chinese).
[157]Jia D C,Hu R Z,Lu Y.Element geochemistry of volcanic rock and discussion on source characteristics in Rucheng ba-sin,Southeast Hunan[J].Geoscience,2003,17(2):131-136(in Chinese).
[158]Xu D R,He Z L,Li P C,et al.Discovery of Late Yans-hanian splitic basalt andits geological significance in North-east Hunan[J].Scientia Geologica Sinica,2006,41(2):311-332(in Chinese).
[159]Peng T P,Wang YJ,Peng B X,et al.Geochemistry char-acteristics andits original significance of Paleogene basalt in Yingjiashan,Northeast Hubei[J].Geochemistry,2006,35(4):395-404(in Chinese).
[160]Wang Y M,Wan T F.Lithosphere tectonic detachment,magmatism and earthquake in Eastern China of Cenozoic[J].Geoscience,2008,22(2):199-221(in Chinese).
[161]Wan T F.Crust rotation in Jurassic and transformation of lithosphere of Eastern China[J].Geological Bulletin of Chi-na,2004,23(9-10):969-972(in Chinese).
[162]Zhou X H.Major transformation of subcontinental litho-sphere beneath Eastern China in the Cenozoic-Mesozoic:re-view and prospect[J].Earth Science Frontiers,2006,13(2):50-64(in Chinese).
[163]Deng J F,Zhao H L,Wu Z X,et al.A mantle plume be-neath the north part of China continent and lithosphere mo-tion[J].Geoscience,1992,6(3):267-274(in Chinese).
[164]Deng J F,Zhao H L,Mo X X,et al.Continental roots-plume tectonics of China—key to the continental dynamics[M].Beijing:Geological Publishing House,1996:1-105(in Chinese).
[165]Lu F X,Zheng J P,Li WP,et al.The main evolution pat-tern of Phanerozoic mantleinthe Eastern China:the“mush-roomcloud”model[J].Earth Science Frontiers,2000,7(1):97-107(in Chinese).
[166]Zhou X M,Li WX.Origin of Late Mesozoic igneous rocks in southeastern China:i mplications for lithosphere subduc-tion and underplating of mafic magmas[J].Tectonophysics,2000,326(3-4):269-287.
[1]万天丰.中国大地构造学纲要[M].北京:地质出版社,2004:1-387.
[2]滕吉文,曾融生,闫雅芬.东亚大陆及周边海域Moho界面深度分布和基本格局[J].中国科学:D辑,2002,32(2):89-100.
[3]刘光鼎.中国大陆构造格架的动力学演化[J].地学前缘,2007,14(3):39-46.
[4]蔡学林,朱介寿,曹家敏,等.东亚西太平洋巨型裂谷体系岩石圈与软流圈结构及动力学[J].中国地质,2002,29(3):234-245.
[5]朱介寿.欧亚大陆及边缘海岩石圈的结构特性[J].地学前缘,2007,14(3):1-20.
[6]路凤香,吴其反.中国东部典型地区下部岩石圈组成、结构和层圈相互作用[M].武汉:中国地质大学出版社,2005:1-195.
[7]石油地质志编写组.大庆油田[M]∥翟光明.石油地质志,卷二(上).北京:石油工业出版社,1993:34-40.
[8]王凯红,裴福萍,冯玉生,等.延边明月沟盆地中生代火山岩深源捕虏体和捕虏晶的发现及矿物化学[J].吉林地质,2005,24(2):21-27.
[9]赵全国,许文良,靳克,等.延边地区中生代火山岩的岩浆源区:来自Sr-Nd同位素和深源捕虏体(晶)的证据[J].吉林大学学报:地球科学版,2005,35(4):416-422.
[10]孙德有,吴福元,林强,等.张广才岭燕山早期白石山岩体成因与壳幔相互作用[J].岩石学报,2001,17(2):227-235.
[11]林强,葛文春,吴福元,等.大兴安岭中生代花岗岩类的地球化学[J].岩石学报,2004,20(3):403-412.
[12]尹志刚,张跃龙,杨晓平,等.大兴安岭北部中生代火山岩特征及岩浆演化[J].世界地质,2006,25(2):120-128.
[13]薛钢,骆剑英,刘金玉.大兴安岭中南段中生代火山岩特征及成因[J].内蒙古科技与经济,2006,4:100-102.
[14]肖成东,张忠良,赵利青.东蒙地区燕山期花岗岩Nd、Sr、Pb同位素及其岩石成因[J].中国地质,2004,31(1):57-63.
[15]陈义贤,陈文寄,周新华,等.辽西及邻区中生代火山岩[M].北京:地震出版社,1997.
[16]邵济安,翟明国,张履桥,等.晋冀蒙交界地区五期岩墙群的界定及其构造意义[J].地质学报,2005,79(1):56-67.
[17]洪大卫,王涛,童英.华北地台和秦岭—大别—苏鲁造山带的中生代花岗岩与深部地球动力学过程[J].地学前缘,2003,10(3):231-256.
[18]阎国翰,许保良,牟保磊,等.太行山—大兴安岭东麓碱性侵入岩年代学和锶、钕、铅同位素特征及其意义[J].地质学报,2000,74(4):774-781.
[19]魏俊浩,刘丛强,唐红峰.辽东五龙地区燕山期侵入岩类同源岩浆演化微量元素、同位素证据与金矿成矿[J].地质论评,2003,49(3):265-271.
[20]张旗,赵太平,王焰,等.中国东部燕山期岩浆活动的几个问题[J].岩石矿物学杂志,2001,20(3):273-280,292.
[21]姜耀辉,蒋少涌,赵葵东,等.辽东半岛煌斑岩SHRI MP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约[J].科学通报,2005,50(19):2161-2168.
[22]汪洋,邓晋福.冀晋辽地区燕山期强过铝质侵入岩岩石化学特征及其动力学意义[J].地质通报,2002,21(4-5):270-276.
[23]吴利仁.华东及邻区中、新生代火山岩[M].北京:科学出版社,1984.
[24]陈志宏,陆松年,李怀坤,等.秦岭造山带富水中基性侵入杂岩的成岩时代——锆石U-Pb及全岩Sm、Nd同位素年代学新证据[J].地质通报,2004,23(4):322-328.
[25]张宏,袁洪林,胡兆初,等.冀北滦平地区中生代火山岩中单颗粒锆石的稀土元素特征及启示[J].中国稀土学报,2006,24(2):227-234.
[26]许文良,林景仟.河北邯邢地区角闪闪长岩中地幔纯橄岩包体的发现与研究[J].地质学报,1991,65(1):33-41.
[27]李伍平,李献华.燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报,2004,20(3):247-254.
[28]牛树银,陈路,许传诗,等.太行山区地壳演化及成矿规律[M].北京:地震出版社,1994:1-203.
[29]万天丰,Teyssier C,曾华霖,等.山东玲珑花岗质岩体侵位机制[J].中国科学:D辑,2000,30(4):337-344.
[30]罗振宽,苗来成.胶东招莱地区花岗岩和金矿床[M].北京:冶金工业出版社,2002:20-57.
[31]郭敬辉,陈福坤,张晓曼,等.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞-碰撞后构造过程:锆石U-Pb年代学[J].岩石学报,2005,21(4):1281-1301.
[32]孙丰月.胶东地区中新生代区域构造演化与成矿[J].长春地质学院学报,1994,24(4):378-384.
[33]陈光远,孙岱生,周若,等.胶东郭家岭花岗闪长岩成因矿物学与金矿化[M].武汉:中国地质大学出版社,1993:1-230.
[34]石油地质志编写组.胜利油田[M]∥翟光明.石油地质志,卷六.北京:石油工业出版社,1993:264-271.
[35]曾键年,左大华,马宪.山西塔儿山地区燕山期岩浆演化及其对金属成矿的控制作用[J].华北地质矿产杂志,1997,12(1):33-43.
[36]真允庆.五台山—恒山一带金、银多金属矿床同位素地球化学及其成矿模型[J].桂林工学院学报,2004,24(2):127-136.
[37]山西地质矿产局.山西省区域地质志[M].北京:地质出版社,1989:1-780.
[38]李曙光,黄方,李晖.大别—苏鲁造山带碰撞后的岩石圈拆离[J].科学通报,2001,46(17):1487-1491.
[39]管运才,吴海权.白马尖超单元组合特征及其成因机制[J].安徽地质,1997,7(2):26-35.
[40]南京大学地质学系.华南不同时代花岗岩类及其与成矿关系[M].北京:科学出版社,1981.
[41]杜杨松,秦新龙,李铉具.安徽铜陵地区中生代幔源岩浆底侵作用——来自矿物巨晶和岩石包体的证据[J].岩石矿物学杂志,2004,23(2):109-116.
[42]王元龙,王焰,张旗.铜陵地区中生代中酸性侵入岩的地球化学特征及其成矿-地球动力学意义[J].岩石学报,2004,20(2):325-338.
[43]楼亚儿,杜杨松.安徽繁昌—铜陵中生代侵入岩的黑云母特征和成因探讨[J].矿物学报,2006,26(2):175-180.
[44]王彦斌,刘敦一,曾普胜,等.安徽铜陵地区幔源岩浆底侵作用的时代——朝山辉石闪长岩锆石SHRI MP定年[J].地球学报,2004,25(4):423-427.
[45]许文良,王清海,王冬燕,等.华北克拉通东部中生代岩石圈减薄的过程与机制:中生代火成岩河深源捕虏体证据[J].地学前缘,2004,11(3):309-317.
[46]翟裕生,姚书振,周若,等.长江中下游铁铜(金)成矿规律[M].北京:地质出版社,1992:1-235.
[47]周泰禧,陈江峰,李学明,等.安徽省印支期岩浆活动质疑[J].岩石学报,1988(3):46-53.
[48]王德滋,周新民,舒良树,等.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化[M].北京:科学出版社,2002.
[49]李永军,谢其山,孪新东,等.西秦岭糜署岭岩浆带成因及构造意义[J].新疆地质,2004,22(4):374-377.
[50]刘埃平,金景福.牧护关花岗岩中锆石标型特征研究[J].地质地球化学,1996,4:15-20.
[51]尚瑞钧,严阵,黄云玉,等.秦巴花岗岩[M].武汉:中国地质大学出版社,1988.
[52]胡海珠,李毅.豫西熊耳山地区燕山期岩浆作用对金银成矿的制约因素[J].矿产与地质,2006,20(4-5):427-429.
[53]严阵,许全成,张海军,等.陕西省花岗岩[M].西安:西安交通大学出版社,1985.
[54]杨起,吴冲龙,汤达祯,等.中国煤变质作用[M].北京:煤炭工业出版社,1996:1-212.
[55]朱介寿,蔡学林,曹家敏,等.中国华南及东海地区岩石圈三维结构及演化[M].北京:地质出版社,2005:1-308.
[56]高天钧,王振民,吴克隆,等.台湾海峡及其周边地区构造岩浆演化与成矿作用[M].北京:地质出版社,1999:1-203.
[57]李向前,陈炯达,潘明宝,等.江苏赣榆城头地区中生代侵入岩石谱系单位划分[J].江苏地质,1999(2):80-83.
[58]周若,杨静,任进.苏州地区I-A型花岗岩特征与成因的对比研究[J].地球科学,1997,22(3):240-246.
[59]周涛发,袁峰,侯明金,等.江南隆起带东段皖赣相邻区燕山期花岗岩类的成因及形成的地球动力学背景[J].矿物岩石,2004,24(3):65-71.
[60]蒋国豪,胡瑞忠,谢桂青,等.大吉山花岗岩体黑云母地球化学特征及其成岩成矿意义[J].矿物岩石,2005,25(5):58-61.
[61]陈培荣,华仁民,章邦桐,等.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学:D辑,2002,45(8):755-768
[63]陈小明,陆建军,刘昌实,等.桐庐、相山火山-侵入杂岩单颗粒锆石U-Pb年龄[J].岩石学报,1999,15(2):272-278.
[64]凌洪飞,沈渭洲,黄小龙.福建省花岗岩类Nd-Sr同位素特征及其意义[J].岩石学报,1999,15(2):255-262.
[65]罗小洪.九瑞地区中生代岩浆活动及其大地构造意义[J].东华理工学院学报,2006,29(2):121-126.
[66]余心起,舒良树,邓国辉,等.江西吉泰盆地碱性玄武岩的地球化学特征及其构造意义[J].现代地质,2005,19:133-140.
[67]赖章忠,王安诚.赣南中生代火山活动时代及岩浆来源[J].江西地质,1996,10:111-118.
[68]周金城,蒋少涌,王孝磊,等.华南中侏罗世玄武岩的岩石地球化学研究——以福建藩坑玄武岩为例[J].中国科学:D辑,2005,35(10):927-936.
[69]江剑丽.福建晚侏罗世两条性质不同的巨型火山岩带[J].福建地质,2001,20(4):171-176.
[70]张文兰,华仁民,王汝成,等.赣南大吉山花岗岩成岩与钨矿成矿年龄的研究[J].地质学报,2006,80(7):956-962.
[71]吴广宇.广宁花岗岩质杂岩的地质年代学研究[J].广东地质,1986,1:1-22.
[72]叶伯丹.两广云开地区同位素年龄数据及其地质意义[J].广东地质,1989,3:39-55.
[73]崔遥.河台花岗岩同位素地质年代学及成因演化[C]∥第四届全国同位素会议论文(摘要)汇编,1989:58-59.
[74]王联魁,沙连埅,徐文新,等.论花岗岩建造与系列——兼论花岗岩三级成因分类[M].广州:广东科技出版社,2003.
[75]耿红燕,徐夕生,O Reilly S Y,等.粤西白垩纪火山-侵入岩浆活动及其地质意义[J].中国科学:D辑,2006,36(7):601-617.
[76]华仁民.南岭中生代陆壳重熔型花岗岩类成岩-成矿的时间差及其地质意义[J].地质论评,2005,51(6):27-33.
[77]张树明,巫建华,周维勋,等.南岭东段燕山期镁铁质岩石Nd-Sr同位素研究[J].东华理工学院学报,2004,27(2):129-135.
[78]马铁球,邝军,柏道远,等.南岭中段诸广山南体燕山早期花岗岩地球化学特征及其形成的构造环境分析[J].中国地质,2006,33(1):119-131.
[79]陈培荣,周新民,张文兰,等.南岭东段燕山早期正长岩-花岗岩杂岩的成因和意义[J].中国科学:D辑,2004,34(6):493-503.
[81]付建明,马昌前,谢才富,等.湖南金鸡岭铝质A型花岗岩的厘定及构造环境分析[J].地球化学,2005,34(3):215-226.
[83]孔华,马芳,黄德志.湖南地区深部岩石剖面的建立——来自深源岩石包体的证据[J].桂林工学院学报,2001,21(3):195-201.
[84]陈必河,贾宝华,刘耀荣,等.湘南中生代火山岩中尖晶石二辉橄榄岩包体Sm-Nd等时线年龄及地质意义[J].地质论评,2004(2):180-183.
[85]顾晟彦,华仁民,戚华文.广西姑婆山花岗岩单颗粒锆石LA-ICP-MS U-Pb定年及全岩Sr-Nd同位素研究[J].地质学报,2006,80(4):543-553.
[86]郭新生,陈江峰,张巽,等.桂东南富钾岩浆杂岩的Nd同位素组成:华南中生代地幔物质上涌事件[J].岩石学报,2001,17(1):19-27.
[87]王建辉,蒋柏昌,孔祥伟,等.姑婆山复式岩体的基本特征及其与成矿作用的关系[J].矿产与地质,2006,20(1):47-53.
[88]曾华霖,刘军,张庆合.华南地区重磁资料处理解释及其在华南地壳结构研究中的应用[M]∥岩石圈构造与动力学开放研究实验室,1994年年报.北京:地震出版社,1995:87-101.
[89]战明国.华南中生代构造-岩浆-成矿作用及区域成矿规律研究[D].宜昌:中国地质科学院宜昌地质矿产研究所,1994.
[90]陈祥,肖力.内蒙古额仁陶勒盖银矿床地球化学研究[J].贵金属地质,1999,8(3):171-178.
[91]邵济安,贾文,储著银等.内蒙古喀喇沁早白垩世橄辉云煌岩岩筒[J].岩石学报,2003,19(3):429-434.
[92]张宏福,郑建平.华北中生代玄武岩的地球化学特征与岩石成因——以辽宁阜新为例[J].科学通报,2003,48(6):603-609.
[94]路凤香,朱勤文,谢意红,等.英安岩中高压辉石巨晶的发现及其意义[J].地球科学——中国地质大学学报,1996,21(5):541-544.
[95]张辉煌,徐义刚,葛文春,等.吉林伊通—大屯地区晚中生代-新生代玄武岩的地球化学特征及其意义[J].岩石学报2006,22(6):1579-1596.
[96]刘若新,陈文寄,解广轰,等.中国新生代火山岩年代学与地球化学[M].北京:地震出版社,1992.
[97]张星.吉林省四平山门早白垩世流纹岩地质特征[J].吉林地质,2001,20(3):30-34.
[98]郑常青,许文良,王冬艳.辽西阜新中生代玄武岩中深源捕虏体的岩石学和矿物化学研究[J].岩石学报,1999,15(4):616-622.
[99]邵济安,李之彤,张履桥.辽西及邻区中-新生代火山岩的时空对称分布及其启示[J].地质科学,2004,39(1):98-106.
[100]张招崇,李兆鼐,王富宝,等.辽西义县盆地火山岩的基本特征及其成因探讨[J].现代地质,1994,8(4):441-451.
[101]邵济安,张履桥,魏春景,等.北京南口中生代双峰式岩墙群的组成及其特征[J].地质学报,2001,75(2):205-212.
[102]苏尚国,邓晋福,赵国春.北京燕山地区薛家石梁杂岩体特征、成因、源区性质及岩石圈减薄方式[J].地学前缘,2006,13(2):148-157.
[103]蔡剑辉,阎国翰,牟保磊,等.北京房山岩体锆石U-Pb年龄和Sr、Nd、Pb同位素与微量元素特征及成因探讨[J].岩石学报,2005,21(3):776-788.
[104]邵济安,李献华,张履桥,等.南口—古崖居中生代双峰式岩墙群形成机制的地球化学制约[J].地球化学,2001,30(6):517-524.
[105]石油地质志编写组.大港油田[M]∥翟光明.石油地质志,卷四.北京:石油工业出版社,1991:92-95.
[106]陈斌,刘超群,田伟.太行山中生代岩浆作用过程中的壳幔岩浆混合作用:岩石学和地球化学证据[J].地学前缘,2006,13(2):140-147.
[107]张勇,陈斌,邵济安,等.华北太行晚中生代煌斑岩地球化学特征及成因探讨[J].岩石矿物学杂志,2003,22(1):29-33.
[108]孟繁聪,李天福,薛怀民,等.胶莱盆地晚白垩世不同地幔源区的两种基性岩浆——诸城玄武岩和胶州玄武岩的对比[J].岩石学报,2006,22(6):1644-1656.
[109]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩及其中幔源包体的岩石学和地球化学研究[J].岩石学报,2005,21(1):99-110.
[112]闫峻,陈江峰,榭智,等.鲁东晚白垩世玄武岩中的幔源捕虏体:对中国东部岩石圈减薄时间制约的新证据[J].科学通报,2003,48(14):1570-1574.
[113]刘晓煌,王金荣,孙兴丽,等.招掖金矿区带花岗岩与金成矿作用研究[J].有色金属,2006,58(4):15-20.
[114]裴福萍.鲁西费县中生代玄武岩及幔源捕掳晶的矿物化学:对岩石圈地幔性质的制约[J].高校地质学报,2004,10(1):88-97.
[115]王冬艳,许文良,兰翔,等.鲁西中生代辉长闪长岩中辉石岩捕虏体的岩石成因[J].吉林大学学报:地球科学版,2004,34(2):167-173.
[116]万天丰.山东省构造演化和应力场研究[J].山东地质,1992,8(2):70-101.
[117]李晓勇,范立勇.西秦岭地区晚中生代OIB型玄武岩的发现及其意义[J].中山大学学报:自然科学版,2006,45(3):127-128.
[118]李家振,张爱民.北淮阳金寨—苏仙石地区中生代花岗岩的成因类型及岩浆演化特征[J].现代地质,1997,11(2):253-260.
[119]李曙光,黄方,李晖.大别—苏鲁造山带碰撞后的岩石圈拆离[J].科学通报,2001,46(17):1487-1491.
[120]王强,赵振华,简平,等.华南腹地白垩纪A型花岗岩类或碱性侵入岩年代学及其对华南晚中生代构造演化的制约[J].岩石学报,2005,21(3):795-808.
[121]马昌前,杨坤光,许长海,等.大别山中生代钾质岩浆作用与超高压变质地体的剥露机理[J].岩石学报,1999,15(3):379-395.
[122]翟建平.昆山、城山和大龙山岩体的锶同位素特征及其成因研究[J].地球化学,1989,3:202-209.
[123]张德全,徐洪林.长江中下游花岗岩类地质地球化学对比研究[J].华南地质与矿产,2002,3:66-77.
[124]邢凤鸣,徐祥.安徽两条A型花岗岩带[J].岩石学报,1994,10(4):357-369.
[125]邢凤鸣.安徽沿江地区中生代岩浆的基本特点[J].岩石学报,1995,11(4):409-422.
[126]李文达,毛建仁,朱云鹤,等.中国东南部中生代火成岩与矿床[M].北京:地震出版社,1998.
[127]邢凤鸣,徐祥.安徽扬子岩浆岩带与成矿[M].合肥:安徽人民出版社,1999:1-170.
[128]靳克,许文良,王清海,等.蚌埠淮光“混合花岗闪长岩”的形成时代及源区:锆石SHRI MP U-Pb地质年代学证据[J].地球学报,2003,24(4):331-335.
[129]杨德彬,许文良,裴福萍,等.蚌埠隆起区花岗岩形成时代及岩浆源区性质:锆石LA-ICPMS U-Pb定年与示踪[J].地球化学,2005,34(5):443-454.
[130]牛漫兰.张八岭隆起南缘早白垩世火山岩稀土元素对比研究[J].中国稀土学报,2006,24(6):739-744.
[131]吴才来,周若,黄许陈,等.安徽茅坦A型花岗岩研究[J].地质学报,1998,72(3):237-247.
[132]章邦桐,张富生,倪琦生,等.安庐石英正长岩带的地质和地球化学特征及成因探讨[J].岩石学报,1988,4(3):1-12.
[133]闫峻,陈江峰,谢智,等.长江中下游地区蝌蚪山晚中生代玄武岩的地球化学研究:岩石圈地幔性质与演化的制约[J].地球化学,2005,34(5):455-469.
[134]戚学祥,旷宏伟,陈培良,等.长江中下游燕山期侵入岩地球化学特征及其地质意义[J].资源调查与环境,2002,23(1):52-59.
[136]陈江峰,Foland K A,刘义茂.苏州复式花岗岩体的精确40Ar/39Ar定年[J].岩石学报,1993,9(1):77-85.
[137]叶水泉.江苏宁镇伏牛山岩体的铷锶等时线年龄[J].江苏地质,1999,23(3):148-150.
[138]龚新法,管建强.浙东南楠溪江中下游地区火山岩地质特征及演化规律[J].浙江地质,1998,14(1):11-17.
[139]陈江峰.简单混合、AFC混合花岗岩同位素数据解释[J].安徽地质,1991,1:19-27.
[140]王中杰,杨琴芳,阮宏宏,等.浙闽赣中生代火山岩地质若干基本问题[J].中国地质科学院南京地质矿产研究所所刊,1987,8(3):1-14.
[141]邱检生,王德滋,McInnes B I A.浙闽沿海地区I型-A型复合花岗岩体的地球化学及成因[J].岩石学报,1999,15(2):237-246
[142]洪大卫,谢锡林,张季生.试析杭州—诸广山—花山高εNd值花岗岩带的地质意义[J].地质通报,2002,21(6):348-354.
[143]周金城,张海进,俞云文.浙江新昌早白垩世复合岩流中岩浆混合作用[J].岩石学报,1994,10(3):236-247.
[144]黄泉祯.1∶500000福建省区域地质图说明书[M].福州:福建地图出版社,1998:1-120.
[145]邱检生,王德滋,McInnes BI.福建沿海铝质A型花岗岩的地球化学及岩石成因[J].地球化学,2000,29(4):313-321.
[146]邱检生,王德滋,周金城.福建永泰云山晚中生代双峰式火山岩的地球化学及岩石成因[J].岩石矿物学杂志,1999,18(2):97-107.
[147]张德全,佘宏全,阎开好,等.福建紫金山地区中生代构造环境转换的岩浆岩地球化学证据[J].地质论评,2001,47(6):608-616.
[148]洪大卫,郭文岐,李戈晶,等.福建沿海晶洞花岗岩带的岩石学和成因演化[M].北京:北京科学技术出版社,1987.
[149]毛建仁,陶奎元,李寄嵎,等.闽西南地区中生代花岗闪长质岩石的特征及其构造演化[J].岩石矿物学杂志,2002,21(2):135-142.
[150]周若,吴克隆.漳州I-A型花岗岩[M].北京:科学出版社,1994.
[151]廖群安,王京名,薛重生,等.江西广丰白垩系盆地中两类玄武岩的特征及其与盆地演化的关系[J].岩石学报,1999,15(1):116-123.
[152]王勇,余达淦.赣东北早白垩世中酸性火山-侵入杂岩微量元素地球化学特征及成因探讨[J].江西地质,2000,14(4):251-255.
[153]余心起,舒良树,颜铁增,等.江山—广丰地区早白垩世晚期玄武岩的岩石地球化学及其构造意义[J].地球化学,2004,33(5):465-474.
[154]王祖伟,周永章,张海华,等.粤西庞西垌银矿床稀土元素地球化学[J].黄金地质,1999,5(2):52-54.
[155]张宗胜.白云嶂中生代晚期碱性火山岩的基本特征与成岩构造环境[J].广东地质,2001,16(4):22-28.
[156]徐夕生,周新民,Reillysy O,等.中国东南下地壳物质与花岗岩成因探索[J].岩石学报,1999,15(2):217-223.
[157]贾大成,胡瑞忠,卢焱.湘东南汝城盆地火山岩的元素地球化学及源区性质讨论[J].现代地质,2003,17(2):131-136.
[158]许德如,贺转利,李鹏春,等.湘东北地区晚燕山期细碧质玄武岩的发现及地质意义[J].地质科学,2006,41(2):311-332.
[159]彭头平,王岳军,彭冰霞,等.湘东北应家山古近纪玄武岩地球化学特征及其成因意义[J].地球化学,2006,35(4):395-404.
[160]王亚妹,万天丰.中国东部新生代岩石圈构造滑脱、岩浆活动和地震[J].现代地质,2008,22(2):199-221.
[161]万天丰.侏罗纪地壳转动与中国东部岩石圈转型[J].地质通报,2004,23(9-10):969-972.
[162]周新华.中国东部中、新生代岩石圈转型与减薄研究若干问题[J].地学前缘,2006,13(2):50-64.
[163]邓晋福,赵海玲,吴宗絮,等.中国北方大陆下的地幔热柱与岩石圈运动[J].现代地质,1992,6(3):267-274.
[164]邓晋福,赵海玲,莫宣学,等.中国大陆根-柱构造——大陆动力学的钥匙[M].北京:地质出版社,1996:1-105.
[165]路凤香,郑建平,李伍平,等.中国东部显生宙地幔演化的主要样式:“蘑菇云”模型[J].地学前缘,2000,7(1):97-107.
①江西地质科学研究所.江西省花岗岩类的基本特征及与钨矿成矿的关系.1983.
①江西地质科学研究所.江西省花岗岩类的基本特征及与钨矿成矿的关系.1983.
[1]Wan T F.An outline of tectonics of China[M].Beijing:Ge-ological Publishing House,2004:1-387(in Chinese).
[2]Teng J W,Zeng R S,Yan Y F.Depth distribution and basic framework of Moho discontinuity in Eastern Asian continent and adjacent sea areas[J].Science in China:Series D,2002,32(2):89-100(in Chinese).
[3]Liu G D.Geodynamical evolution and tectonic framework of China[J].Earth Science Frontiers,2007,14(3):39-46(in Chinese).
[4]Cai X L,Zhu J S,Cao J M,et al.Structure and dynamic of lithosphere and athenosphere of Eastern Asian-Western Pacif-ic giant rift system[J].Geologyin China,2002,29(3):234-245(in Chinese).
[5]Zhu J S.The structural characteristics of lithosphere in the continent of Eurasia and its marginal seas[J].Earth Science Frontiers,2007,14(3):1-20(in Chinese).
[6]Lu F X,Wu Q F.Composition,structure and spheres inter-action of lower lithosphereintypical areas of East China[M].Wuhan:China University of Geosciences Press,2005:1-195(in Chinese).
[7]Compile Group of Petroleum Geology.Daqing oil field[M]∥Zhai G M.Petroleumgeology,Vol.2(Ⅰ).Beijing:Petrole-umIndustry Press,1993:34-40(in Chinese).
[8]Wang K H,Pei F P,Feng YS,et al.Discovered deep source inclusion andinclusion crystal and their mineral-chemistry of Mesozoic volcanic rocks in Mingyuegou Basin,Yanbian[J].Jilin Geology,2005,24(2):21-27(in Chinese).
[9]Zhao Q G,Xu W L,Jin K,et al.Magmatic source area of Mesozoic volcanic rocks in Yanbian area:evidences form Sr-Ndisotope and deep sourceinclusion[J].Journal of Jilin Uni-versity:Earth Science Edition,2005,35(4):416-422(in Chinese).
[10]Sun D Y,Wu F Y,Lin Q,et al.Origin of Baishishanintru-sion and interaction between crust and mantle during Early Yashanianin Zhangguangcailing[J].Acta Petrologica Sinica,2001,17(2):227-235(in Chinese).
[11]Lin Q,Ge W C,Wu F Y,et al.Granitoid geochemistry of Mesozoic in Da Hinggan Ling[J].Acta Petrologica Sinica,2004,20(3):403-412(in Chinese).
[12]Yin Z G,Zhang Y L,Yang X P,et al.Characteristics and magmatic evolution of Mesozoic volcanic rocks at northern Da Hinggan Ling[J].Global Geology,2006,25(2):120-128(in Chinese).
[13]Xue G,Luo J Y,Liu J Y.Mesozoic volcanic rock character-istics and originin middle-southern Da Hinggan Ling[J].Sci-ence,Technology and Economy of Inner Mongolia,2006,4:100-102(in Chinese).
[14]Xiao C D,Zhang Z L,Zhao L Q.Nd,Sr,Pb isotope and rock origin of Yanshanian granite in eastern Inner Mongolia[J].Geology in China,2004,31(1):57-63(in Chinese).
[15]Chen Y X,Chen WJ,Zhou X H,et al.Mesozoic volcanic rock in western Liaoning and adjacent area[M].Beijing:Seismological Press,1997(in Chinese).
[16]Shao J A,Zhai M G,Zhang L Q,et al.Determined dyke swarminfive stages andits tectonic significance at the margin among Shanxi,Hebei andInner Mongolia[J].Acta Geologica Sinica,2005,79(1):56-67(in Chinese).
[17]Hong D W,Wang T,Tong Y.Mesozoic granitoids from North China block and Qinling-Dabie-Sulu orogenic belt and their deep dynamic process[J].Earth Science Frontiers,2003,10(3):231-256(in Chinese).
[18]Yan G H,Xu B L,Mu B L,et al.Alkaline intrusion at the east foot of the Taihang-Da Hinggan Ling:choronology,Sr,Nd and Pbisotopic characteristics and their i mplications[J].Acta Geologica Sinica,2000,74(4):774-781(in Chinese).
[19]Wei J H,Liu C Q,Tang H F.Trace element,isotopic evi-dence in syn-original magmatismof Yanshanianintrusions and gold mineralization at Wulong area of Liaoning[J].Geological Review,2003,49(3):265-271(in Chinese).
[20]Zhang Q,Zhao T P,Wang Y,et al.Some problems of mag-matismin Yanshanian of eastern China[J].Journal of Petrol-ogy and Mineralogy,2001,20(3):273-280,292(in Chi-nese).
[21]Jiang Y H,Jiang S Y,Zhao K D,et al.SHRI MP zircon U-Pb age of lamprophyre at East Liaoning Peninsula and restric-tion of beginningti me for lithosphere thinning of Eastern Chi-na[J].Chinese Science Bulletin,2005,50(19):2161-2168(in Chinese).
[22]Wang Y,Deng J F.Petrochemical characteristics and geody-namic significance of the Yanshanian strongly peraluminous intrusive rocks in the Hebei-Shanxi-Liaoning area[J].Geo-logical Bulletin of China,2002,21(4-5):270-276(in Chi-nese).
[23]Wu L R.Meso-Cenozoic volcanic rocksin East China and ad-jacent areas[M].Beijing:Science Press,1984(in Chinese).
[24]Chen Z H,Lu S N,Li H K,et al.Age of the Fushui inter-mediate-mafic intrusive complex in the Qinling orogen:new zircon U-Pb and whole-rock Smand Ndisotope chronological evidence[J].Geological Bulletin of China,2004,23(4):322-328(in Chinese).
[25]Zhang H,Yuan H L,Hu Z C,et al.Rare earth element characteristics andits significance of single zirconin Mesozoic volcanic rocks,in Luanping of Hebei[J].Journal of Rare Earth Element in China,2006,24(2):227-234(in Chinese).
[26]Xu WL,Lin J Q.The discovery and study of mantle-derived dunite inclusions in hornblende-diorite in the Handan-Xingtai area,Hebei[J].Acta Geologica Sinica,1991,65(1):33-41(in Chinese).
[27]Li WP,Li X H.Origin and its significance of Middle-Late Jurassic intermediate-acid volcanic rocks,in middle Yanshan orogenic zone[J].Acta Petrologica Sinica,2004,20(3):247-254(in Chinese).
[28]Niu S Y,Chen L,Xu C S,et al.The crustal evolution and metallogenic regularity of the Taihangshan Area[M].Bei-jing:Seismological Press,1994:1-203(in Chinese).
[29]Wan T F,Teyssier C,Zeng HL,et al.Emplacement mech-anism of Linglong granitoid complex,Shandong Peninsula,China[J].Science in China:Series D,2001,44(6):535-544(in Chinese).
[30]Luo Z K,Miao L C.Granites and gold depositsin Zhaoyuan-Laizhou Area,Eastern Shandong Province[M].Beijing:Metallurgical Industry Press,2002:20-57(in Chinese).
[31]Guo J H,Chen F K,Zhang X M,et al.Mesozoic magmatic intrusion and syn-collision-post-collision tectonicsin Northern Sulu UHP belt,eastern China:SHRI MP zircon U-Pb geo-chronology[J].Acta Petrologica Sinica,2005,21(4):1281-1301(in Chinese).
[32]Sun F Y.Mesozoic-Cenozoic regional tectonic evolution and mineralizationin Eastern Shandong[J].Journal of Changchun Institute of Geology,1994,24(4):378-384(in Chinese).
[33]Chen G Y,Sun D S,Zhou X R,et al.Genetic mineralogy and gold mineralization of Guojialing granodiorite in Jiaodong region[M].Wuhan:China University of Geosciences Press,1993:1-230(in Chinese).
[34]Compile Group of Petroleum Geology.Shengli oil field[M]∥Zhai G M.Petroleum geology,Vol.6.Beijing:Petroleum Industry Press,1993:264-271(in Chinese).
[35]Zeng J N,Zuo D H,Ma X.Yanshanian magmatic evolution andits influence to metal mineralizationin Ta ershan,Shanxi[J].Journal of Geology and Mineral Resources of North Chi-na,1997,12(1):33-43(in Chinese).
[36]Zhen Y Q.Isotopic geochemistry andits mineralization model of gold,silver,multi-metal ore depositsin Wutaishan-Hengs-han[J].Journal of Technology Institute of Guilin,2004,24(2):127-136(in Chinese).
[37]Shanxi Bureau of Geology and Mineral Resources(Shanxi Ge-ological Survey).Regional geology of Shanxi Province[M].Beijing:Geological Publishing House,1989:1-780(in Chi-nese).
[38]Li S G,Huang F,Li H.Post collision lithosphere detach-ment in Dabie-Sulu orogenic belt[J].Chinese Science Bulle-tin,2001,46(17):1487-1491(in Chinese).
[39]Guan Y C,Wu H Q.Characteristics of Bai majian ultra-unite and its origin[J].Anhui Geology,1997,7(2):26-35(in Chi-nese).
[40]Depart ment of Geology,Nanjing University.South China granitoids and their mineralizations[M].Beijing:Science Press,1981(in Chinese).
[41]Du Y S,Qin X L,Li XJ.Mesozoic mantle source magmatic underplating of Tongling,Anhui—evidences fromgreat crys-tal and rockinclusion[J].Journal of Petrology and Mineralo-gy,2004,23(2):109-116(in Chinese).
[42]Wang Y L,Wang X,Zhang Q.The geochemical characteris-tics of Mesozoic intermediate-acid intrusives of the Tongling area andits metallogenesis-geodynamic i mplications[J].Acta Petrologica Sinica,2004,20(2):325-338(in Chinese).
[43]Lou Y E,Du Y S.Characteristics and original discussion of biotite in Mesozoic intrusion of Fanchang-Tongling,Anhui[J].Journal of Mineralogy,2006,26(2):175-180(in Chi-nese).
[44]Wang Y B,Liu D Y,Zeng P S,et al.Underplating choron-ology of mantle magmain Tongling,Anhui—zircon SHRI MP dating in Chaoshan pyroxene diorite[J].Acta Geoscientica Sinica,2004,25(4):423-427(in Chinese).
[45]Xu WL,Wang Q H,Wang D Y,et al.Mesozoiclithosphere thinning and mechanismof eastern North China Craton:evi-dences of deep inclusion of Mesozoic magmatic rocks[J].Earth Science Frontiers,2004,11(3):309-317(in Chinese).
[46]Zhai Y S,Yao S Z,Zhou X R,et al.Metallogeny of iron,copper and goldin Lower and Middle Reaches of Yangtze Riv-er[M].Beijing:Geological Publishing House,1992:1-235(in Chinese).
[47]Zhou T X,Chen J F,Li X M,et al.Query the Indosinian magmatismin Anhui[J].Acta Petrologica Sinica,1988(3):46-53(in Chinese).
[48]Wang D Z,Zhou X M,Shu L S,et al.Origin of granitic vol-canic-intrusion complex and crustal evolution during Late Mesozoic in Southeast China[M].Beijing:Science Press,2002(in Chinese).
[49]Li YJ,Xie QS,Luan X D,et al.Origin andtectonic signifi-cance of West Qinling Michuling magma belt[J].Xinjiang Geology,2004,22(4):374-377(in Chinese).
[50]Liu A P,Jin J F.Research on zircon typomorphic character-istics in Muhuguan granite[J].Geology and Geochemistry,1996,4:15-20(in Chinese).
[51]Shang RJ,Yan Z,Huang Y Y,et al.Granitein Qinling and Dabashan[M].Wuhan:China University of Geosciences Press,1988(in Chinese).
[52]Hu HZ,Li Y.Restrict factor of Yanshanian magmatismto gold and silver mineralization in Xiong ershan,western Henan[J].Mineralization and Geology,2006,20(4-5):427-429(in Chinese).
[53]Yan Z,Xu Q C,Zhang HJ,et al.Granite in Shaanxi Prov-ince[M].Xi an:Xi an Communication University Press,1985(in Chinese).
[54]Yang Q,Wu C L,Tang D Z,et al.Coal metamorphismin China[M].Beijing:Coal Industry Press,1996:1-212(in Chinese).
[55]Zhu J S,Cai X L,Cao J M,et al.The three-di mensional structure of lithosphere and its evolution in South China and East China Sea[M].Beijing:Geological Publishing House,2005:1-308(in Chinese).
[56]Gao TJ,Wang Z M,Wu K L,et al.Tectono-magmatic evo-lution and metallogeny of Tai wan Strait andits adjacent areas[M].Beijing:Geological Publishing House,1999:1-203(in Chinese).
[57]Li X Q,Chen J D,Pan MB,et al.Petrological suits of Mes-ozoic intrusionin Chengtou area,Ganyu,Jiangsu[J].Jiangsu Geology,1999(2):80-83(in Chinese).
[58]Zhou X R,Yang J,Ren J.Comparative study on the charac-teristics and genesis between I-and A-type granite of Suzhou area[J].Earth Science,1997,22(3):240-246(in Chinese).
[59]Zhou T F,Yuan F,Hou MJ,et al.Origin of Yanshanian granite and geodynamic background in the boundary between Anhui and Jiangxi of Jiangnan Uplift area[J].Journal of Mineralogy and Petrology,2004,24(3):65-71(in Chinese).
[60]Jiang G H,Hu R Z,Xie G Q,et al.Biotite geochemistry characteristics and influences of rock and ore deposit forma-tionin Dajishan granite[J].Journal Mineralogy and Petrolo-gy,2005,25(5):58-61(in Chinese).
[61]Chen P R,Hua R M,Zhang B T,et al.Early Yanshanian post-orogenic granitoids in the Nanling region:petrological constraints and geodynamic settings[J].Science in China:Series D,2002,45(8):755-768(in Chinese).
[62]Li X H,Chen Z G,Liu D Y,et al.Jurassic gabbro-granite-syenite suites fromsouthern Jiangxi Province,SE China:age,origin and tectonic significance[J].International Geological Review,2003,45:898-921.
[63]Chen X M,Lu J J,Liu C S,et al.Single zircon U-Pb age in Tonglu-Xiangshan volcanic-intrusion complex[J].Acta Pet-rologica Sinica,1999,15(2):272-278(in Chinese).
[64]Ling HF,Shen WC,Huang X L.Nd-Sr isotopic character-istics of granitoid and their significances in Fujian[J].Acta Petrologica Sinica,1999,15(2):255-262(in Chinese).
[65]Luo X H.Mesozoic magmatismandits tectonic significancein Jiujiang-Ruichang areas[J].Journal of Institute of Technolo-gy of East China,2006,29(2):121-126(in Chinese).
[66]Yu X Q,Su L S,Deng G H,et al.Geochemistry character-istics andits tectonic significance of alkali basalt in Jitai Ba-sin,Jiangxi[J].Geoscience,2005,19:133-140(in Chi-nese).
[67]Lai Z Z,Wang A C.Mesozoic volcanic activity age and mag-matic sourcein South Jiangxi[J].Jiangxi Geology,1996,10:111-118(in Chinese).
[68]Zhou J C,Jiang S Y,Wang X L,et al.Petrological-geo-chemistry for Middle Jurassicin South China—example to ba-salt of Fankeng in Fujian[J].Science in China:Series D,2005,35(10):927-936(in Chinese).
[69]Jiang J L.Two distinguish macro-volcanic zones of Late Ju-rassic in Fujian[J].Fujian Geology,2001,20(4):171-176(in Chinese).
[70]Zhang WL,Hua R M,Wang R C,et al.Research onforma-tion of granite andforming age of Tungsten ore deposit at Da-jishan,South Jiangxi[J].Acta Geologica Sinica,2006,80(7):956-962(in Chinese).
[71]Wu G Y.Chronology of Guangning granite complex[J].Guangdong Geology,1986,1:1-22(in Chinese).
[72]Ye B D.Isotopic ages andits geological significancein Yunkai area of Guangdong and Guangxi[J].Guangdong Geology,1989,3:39-55(in Chinese).
[73]Cui Y.Isotopic chronology and origin evolution of Hetai granite[C]∥Proceedings of4th China Isotopic Conference,1989:58-59(in Chinese).
[74]Wang L K,Sha L F,Xu WX,et al.Discussion onformation and series of granite—also discussion on three original divi-sions[M].Guangzhou:Guangdong Science and Technology Press,2003(in Chinese).
[75]Geng HY,Xu XS,O Reilly S Y,et al.Cretaceous volcanic-intrusionin western Guangdong andits geological significance[J].Science in China:Series D,2006,36(7):601-617(in Chinese).
[76]Hua R M.Differential ti me between continental crust remelt granite and mineralization,and their geological influence[J].Geological Review,2005,51(6):27-33(in Chinese).
[77]Zhang S M,Wu J H,Zhou WX,et al.Nd-Sr isotopic study for mafic rocks of Yanshanian at eastern Nanling[J].Journal of Institute of Technology of East China,2004,27(2):129-135(in Chinese).
[78]Ma T Q,Kuang J,Bo D Y,et al.Granite geochemistry characteristics and their analysis of formation tectono-envi-ronment at south Zhuguangshan of Middle Nanling[J].Geolo-gy in China,2006,33(1):119-131(in Chinese).
[79]Chen P R,Zhou X M,Zhang WL,et al.Origin and influ-ence of syenite-granite complex of Early Yanshanian at east-ern part of Nanling[J].Science in China:Series D,2004,34(6):493-503(in Chinese).
[80]Gilder S A,Gill J B,Coe R S,et al.Isotopic and paleomag-netic constraints on the Mesozoic tectonic evolution of South China[J].J Geophys Res,1996,101(B7):16137-16155.
[81]Fu J M,Ma C Q,Xie C F,et al.Determined Atype of alumi-nous granite and tectonic environment analysis in Jinjiling of Hu-nan[J].Geochemistry,2005,34(3):215-226(in Chinese).
[82]Li X H,Chung S L,Zhou H W,et al.Jurassic intraplate magmatismin southern Hunan-eastern Guangxi:40Ar/39Ar dating,geochemistry,Sr-Ndisotopes andi mplications for tec-tonic evolution of SE China[M]∥Malpas J,Fletcher C J,Ai-tchison J C,et al.Aspects of the tectonic evolution of China.Geological Society,London,Special Publications,2004,226:193-216.
[83]Kong H,Ma F,Huang D Z.Deep rock sectionin Hunan ar-ea:evidence fromdeep sourceinclusions[J].Journal of Insti-tute of Technology of Guilin,2001,21(3):195-201(in Chi-nese).
[84]Chen B H,Jia B H,Liu Y R,et al.Sm-Nd isochron age of spinel lherzolite inclusionin Mesozoic volcanic rocks of South Hunan[J].Geological Review,2004(2):180-183(in Chi-nese).
[85]Gu C Y,Hua R M,Qi H W.Single zircon LA-ICP-MS U-Pb dating and whole rock Sr-Nd isotopic of Guposhan granite in Guangxi[J].Acta Geologica Sinica,2006,80(4):543-553(in Chinese).
[86]Guo X S,Chen J F,Zhang X,et al.Ndisotopic composition of alkali magmatic complexin southeast Guangxi:South Chi-na Mesozoic mantle material uplift event[J].Acta Petrologica Sinica,2001,17(1):19-27(in Chinese).
[87]Wang J H,Jiang B C,Kong X W,et al.Basic characteristics of Guposhan complexintrusion and relationship with mineral-ization[J].Mineralization and Geology,2006,20(1):47-53(in Chinese).
[88]Zeng H L,Liu J,Zhang Q H.Gravity and magnetic data processing and interpretation and its application to research on crustal structure,South China[M]∥1994Annual Report,Laboratory of Lithosphere Tectonics and Dynamics.Beijing:Seismological Press,1995:87-101(in Chinese).
[89]Zhan M G.Tectonic-magmatism-mineralization and regional metallogenic research of Mesozoic in South China[D].Yichang:Yichang Institute of Geology and Mineral Re-sources,CAGS,1994(in Chinese).
[90]Chen X,Xiao L.Geochemistry research on Erentaolegai sil-ver ore deposit,Inner Mongolia[J].Precious Metal Geology,1999,8(3):171-178(in Chinese).
[91]Shao J A,Jia W,Chu Z Y,et al.Early Cretaceous olivine-pyroxene minette volcanic pipe in Karaxin,Inner Mongolia[J].Acta Petrologica Sinica,2003,19(3):429-434(in Chi-nese).
[92]Zhang H F,Zheng J P.Geochemistry characteristics and rock origin for Mesozoic basalt in North China—case of Fux-in,Liaoning[J].Chinese Science Bulletin,2003,48(6):603-609(in Chinese).
[93]Lu F X,Zhu Q W,Li S T,et al.Mesozoic volcanismsur-rounding Songliao basin,China:i mplication for the relation-ship with evolution of basin[J].Journal of China University of Geosciences,1997,8(1):72-77.
[94]Lu F X,Zhu Q W,Xie Y H,et al.Discovery of giant crystal of high pressure pyroxene in dacite and its significance[J].Earth Science—Journal of China University of Geosciences,1996,21(5):541-544(in Chinese).
[95]Zhang H H,Xu Y G,Ge W C,et al.Basalt geochemistry characteristic andits significance during Late Mesozoic-Ceno-zoic in Yitong-Datun areas,Jilin[J].Acta Petrologica Sinica,2006,22(6):1579-1596(in Chinese).
[96]Liu R X,Chen WJ,Xie G H,et al.Chronology and geo-chemistry of Cenozoic volcanic rocks in China[M].Beijing:Seismological Press,1992(in Chinese).
[97]Zhang X.Geological characteristics of Early Cretaceous rhyo-lite in Shanmen,Siping,Jilin[J].Jilin Geology,2001,20(3):30-34(in Chinese).
[98]Zheng C Q,Xu WL,Wang D Y.The petrology and mineral chemistry of deep-seated xenolithsin Mesozoic basalt in Fuxin district from western Liaoning[J].Acta Petrologica Sinica,1999,15(4):616-622(in Chinese).
[99]Shao J A,Li Z T,Zhang L Q.Ti me and space symmetry dis-tribution and significance of Mesozoic-Cenozoic volcanic rocks in western Liaoning and its adjacent areas[J].Scientia Geo-logica Sinica,2004,39(1):98-106(in Chinese).
[100]Zhang Z C,Li Z N,Wang F B,et al.Basic characteristic of volcanic rock andits origin in Yixian Basin,western Liaon-ing[J].Geoscience,1994,8(4):441-451(in Chinese).
[101]Shao J A,Zhang L Q,Wei CJ,et al.The composition and its characteristics of bi modal dyke swarm of Mesozoic at Nankou,Beijing[J].Acta Geologica Sinica,2001,75(2):205-212(in Chinese).
[102]Su S G,Deng J F,Zhao G C.Characteristics,origin,source region and thinning type of lithosphere Xuejiashiliang complex[J].Earth Science Frontiers,2006,13(2):148-157(in Chinese).
[103]Cai J H,Yan G H,Mu B L,et al.Zircon U-Pb age,Sr-Nd-Pbisotopic,trace elements and discussion on its origin[J].Acta Petrologica Sinica,2005,21(3):776-788(in Chi-nese).
[104]Shao J A,Li X H,Zhang L Q,et al.Geochemical condition for genetic mechanismof the Mesozoic bi modal dike swarms in Nankou-Guyaju[J].Geochi mica,2001,30(6):517-524(in Chinese).
[105]Compile Group of Petroleum Geology.Dagang oil field[M]∥Zhai G M.Petroleumgeology,Vol.4.Beijing:Petroleum Industry Press,1991:92-95(in Chinese).
[106]Chen B,Liu C Q,Tian W.Crust-mantle magma migmatiti-zation during Mesozoic in Taihangshan:evidences of petrol-ogy and geochemistry[J].Earth Science Frontiers,2006,13(2):140-147(in Chinese).
[107]Zhang Y,Chen B,Shao J A,et al.Geochemistry character-istics and discussion on origin for Late Mesozoic lampro-phyre in Taihangshan,North China[J].Journal of Mineral-ogy and Petrology,2003,22(1):29-33(in Chinese).
[108]Meng F C,Li T F,Xue H M,et al.Contrast withtwo Late Cretaceous basic magma(Zhucheng and Jiaozhou basalts,in Jiaolai Basin)formed in different mantle sources[J].Acta Petrologica Sinica,2006,22(6):1644-1656(in Chinese).
[109]Yan J,Chen J F,Xie Z,et al.Research on petrology and geochemistry of Late Cretaceous basalt and mantle inclusion in East Shandong[J].Acta Petrologica Sinica,2005,21(1):99-110(in Chinese).
[110]Zhang H F,Sun M.Geochemistry of Mesozoic basalts and mafic dikes,southeastern north china craton and tectonic i mplications[J].International Geological Review,2002,44:370-382.
[111]Zhang HF,Sun M,Zhou X H,et al.Secular evolution of the lithosphere beneaththe eastern North China Craton:ev-idence from Mesozoic basalts and high-Mg andesites[J].Geochi mica et Cosmochi mica Acta,2003,67(22):4373-4387.
[112]Yan J,Chen J F,Xie Z,et al.Mantle source inclusion of Late Cretaceous basalt in East Shandong:new evidence for ti me restrain of Eastern China lithosphere thinning[J].Chi-nese Science Bulletin,2003,48(14):1570-1574(in Chi-nese).
[113]Liu X H,Wang J R,Sun X L,et al.Research on granite and gold mineralization in Zhaoyuan-Yexian ore fields[J].Nonferrous Metal,2006,58(4):15-20(in Chinese).
[114]Pei F P.Mesozoic basalt and mineral-chemistry of crystal inclusion of mantle source:restrict to character of litho-sphere mantle[J].Journal of Geology of Universities,2004,10(1):88-97(in Chinese).
[115]Wang D Y,Xu WL,Lan X,et al.Origin of pyroxenite in-clusionin Mesozoic gabbro-diorite of Western Shandong[J].Journal of Jilin University:Earth Science Edition,2004,34(2):167-173(in Chinese).
[116]Wan T F.Tectonic evolution and stress fields of Shandong Province[J].Geology of Shandong,1992,8(2):70-101(in Chinese).
[117]Li X Y,Fan L Y.Discovery and its significance of Late Mesozoic OIBtype basalt in Western Qinling[J].Journal of Zhongshan University:Natural Science Edition,2006,45(3):127-128(in Chinese).
[118]Li J Z,Zhang A M.Original type and magmatic evolution characteristics of Mesozoic granite in Jinzhai-Suxian area of Northern Huaiyang[J].Geoscience,1997,11(2):253-260(in Chinese).
[119]Li S G,Huang F,Li H.Post-collision lithosphere detach-ment in Dabie-Sulu orogenic belt[J].Chinese Science Bulle-tin,2001,46(17):1487-1491(in Chinese).
[120]Wang Q,Zhao Z H,Jian P,et al.Chronology of Creta-ceous Atype granitoid or alkali intrusion in inland of South China and restrain for Late Mesozoic tectonic evolution in South China[J].Acta Petrologica Sinica,2005,21(3):795-808(in Chinese).
[121]Ma C Q,Yang K G,Xu C H,et al.Mesozoic Alkali mag-matism in Dabieshan and uplift mechanism of ultra-high pressure metamorphic block[J].Acta Petrologica Sinica,1999,15(3):379-395(in Chinese).
[122]Zhai J P.Sr isotopic characteristics and origin research of Kunshan,Chengshan and Dalongshan intrusions[J].Geo-chemistry,1989,3:202-209(in Chinese).
[123]Zhang D Q,Xu H L.Compare research on geology-geo-chemistry of granitoid in lower and middle reaches of Yan-gtze River[J].South China Geology and Resources,2002,3:66-77(in Chinese).
[124]Xing F M,Xu X.Two Atype granite zones in Anhui[J].Acta Petrologica Sinica,1994,10(4):357-369.
[125]Xing F M.Basic characteristics of Mesozoic magma along Yangtze River in Anhui[J].Acta Petrologica Sinica,1995,11(4):409-422.
[126]Li W D,Mao J R,Zhu Y H,et al.Mesozoic magmatism and ore deposits of Southeast China[M].Beijing:Seismo-logical Press,1998(in Chinese).
[127]Xing F M,Xu X.Magma rock zone and mineralization in Yangtze of Anhui[M].Hefei:People Publishing House of Anhui,1999:1-170(in Chinese).
[128]Jin K,Xu W L,Wang Q H,et al.Formation ti me and source area of grano-diorite in Huaiguang,Benfu:zircon SHRI MP U-Pb chronology evidence[J].Acta Geoscientica Sinica,2003,24(4):331-335(in Chinese).
[129]Yang D B,Xu WL,Pei F P,et al.Granite formation age and feature of magma source area for Benfu area:zircon LA-ICPMS U-Pb age dating and tracing[J].Geochemistry,2005,34(5):443-454(in Chinese).
[130]Niu ML.Compare research on rare earth elements of Early Cretaceous volcanic rockin south margin of Zhangbaling up-lift area[J].Journal of Rare Earth Element in China,2006,24(6):739-744(in Chinese).
[131]Wu C L,Zhou X R,Huang X C,et al.Research on Atype granite in Maotan,Anhui[J].Acta Geologica Sinica,1998,72(3):237-247(in Chinese).
[132]Zhang B T,Zhang F S,Ni QS,et al.Discussion on geolo-gy and geochemistry characteristics and originin quartz sye-nite zone of Anqing-Lujiang area[J].Acta Petrologica Sini-ca,1988,4(3):1-12(in Chinese).
[133]Yan J,Chen J F,Xie Z,et al.Geochemistry research of Late Mesozoic basalt in Kedoushan,lower and middle rea-ches of Yangtze River:mantle feature of lithosphere and e-volution restrain[J].Geochemistry,2005,34(5):455-469(in Chinese).
[134]Qi X X,Kuang H W,Chen P L,et al.Geochemistry char-acteristics and its geological significance of Yanshanian in-trusion in lower and middle reaches of Yangtze River[J].Resource Survey and Environment,2002,23(1):52-59(in Chinese).
[135]Xu W L,Wang Q H,Liu X C,et al.Chronology and sources of Mesozoic intrusive complex in Xu-Huai region,central China:constraints fromSHRI MPzircon U-Pb dating[J].Acta Geologica Sinica,2004,78(1):96-106.
[136]Chen J F,Foland K A,Liu Y M.Actural40Ar/39Ar age dating of granite complex in Suzhou[J].Acta Petrologica Sinica,1993,9(1):77-85(in Chinese).
[137]Ye S Q.Rb-Sr isochron age of Funiushanintrusionin Nan-jing-Zhenjiang,Jiangsu[J].Jiangsu Geology,1999,23(3):148-150(in Chinese).
[138]Gong X F,Guan J Q.Volcanic geological characteristics and evolutioninlower and middle reaches of Nanxijiang,South-east Zhejiang[J].Zhejiang Geology,1998,14(1):11-17(in Chinese).
[139]Chen J F.Explanation of isotopic data of si mple-mixed,AFC migmatite granite[J].Anhui Geology,1991,1:19-27(in Chinese).
[140]Wang Z J,Rang Q F,Ruan H H,et al.Some basic prob-lems of Mesozoic volcanic geologyin Zhejiang-Fujian-Jiangxi[J].Journal of Nanjing Institute of Geology and Resources,1987,8(3):1-14(in Chinese).
[141]Qiu J S,Wang D Z,McInnes BI A.Geochemistry and ori-gin of I and Atypes granite complex in coastal of Zhejiang and Fujian[J].Acta Petrologica Sinica,1999,15(2):237-246(in Chinese).
[142]Hong D W,Xie X L,Zhang J S.The geological significance of highεNdvalue granitic zone for Hangzhou-Zhuguangshan-Huashan[J].Geological Bulletin of China,2002,21(6):348-354(in Chinese).
[143]Zhou J C,Zhang HJ,Yu Y W.Magma migmatization in complex flowof Early Cretaceousin Xinchang,Zhejiang[J].Acta Petrologica Sinica,1994,10(3):236-247(in Chi-nese).
[144]Huang Q Z.Explanation of regional geological map of Fu-jian Province(1∶500000)[M].Fuzhou:Catastrophy Pub-lishing House of Fujian,1998:1-120(in Chinese).
[145]Qiu J S,Wang D Z,McInnes BI.Geochemistry and origin of aluminium Atype granite in coastal of Fujian[J].Geo-chemistry,2000,29(4):313-321(in Chinese).
[146]Qiu J S,Wang D Z,Zhou J C.Geochemistry and rock ori-gin of bi modal volcanic rocks during Late Mesozoic in Yun-shan,Yongtai,Fujian[J].Journal of Petrology and Miner-alogy,1999,18(2):97-107(in Chinese).
[147]Zhang D Q,She H Q,Yan K H,et al.Magmatic geochem-istry evidences for Mesozoic tectonic environments change at Zijinshan area of Fujian[J].Geological Review,2001,47(6):608-616(in Chinese).
[148]Hong D W,Guo W Q,Li GJ,et al.Miarolitic granite pe-trology and original evolution at coastal of Fujian[M].Bei-jing:Beijing Science and Technology Press,1987(in Chi-nese).
[149]Mao J R,Tao K Y,Li J Y,et al.Mesozoic grano-diorite characteristics andits tectonic evolutionin Southwest Fujian[J].Journal of Petrology and Mineralogy,2002,21(2):135-142(in Chinese).
[150]Zhou X R,Wu K L.I-Atype granite in Zhangzhou[M].Beijing:Science Press,1994(in Chinese).
[151]Liao Q A,Wang J M,Xue Z S,et al.Characteristics of two type basalts in Cretaceous basins of Guangfeng,Jiangxi and its relationship of basin evolution[J].Acta Petrologica Sini-ca,1999,15(1):116-123(in Chinese).
[152]Wang Y,Yu D G.Trace elements geochemistry characteris-tics and origin of intermediate-acid volcano-intrusion com-plex of Early Cretaceous in Northeast Jiangxi[J].Jiangxi Geology,2000,14(4):251-255(in Chinese).
[153]Yu X Q,Shu L S,Yan T Z,et al.Rock geochemistry and its tectonic significance of Early Cretaceous basalt in Jiangs-han-Guangfeng areas[J].Geochemistry,2004,33(5):465-474(in Chinese).
[154]Wang Z W,Zhou Y Z,Zhang H H,et al.Rare earth ele-ments geochemistry of silver deposit in Panxidong,western Guangdong[J].Gold Geology,1999,5(2):52-54(in Chi-nese).
[155]Zhang Z S.Basic characteristics and formation environment of Late Mesozoic alkali volcanic rock in Baiyuanzhang[J].Guangdong Geology,2001,16(4):22-28(in Chinese).
[156]Xu X S,Zhou X M,Reillysy O,et al.Lower crust material of Southeast China and discussion on origin[J].Acta Petro-logica Sinica,1999,15(2):217-223(in Chinese).
[157]Jia D C,Hu R Z,Lu Y.Element geochemistry of volcanic rock and discussion on source characteristics in Rucheng ba-sin,Southeast Hunan[J].Geoscience,2003,17(2):131-136(in Chinese).
[158]Xu D R,He Z L,Li P C,et al.Discovery of Late Yans-hanian splitic basalt andits geological significance in North-east Hunan[J].Scientia Geologica Sinica,2006,41(2):311-332(in Chinese).
[159]Peng T P,Wang YJ,Peng B X,et al.Geochemistry char-acteristics andits original significance of Paleogene basalt in Yingjiashan,Northeast Hubei[J].Geochemistry,2006,35(4):395-404(in Chinese).
[160]Wang Y M,Wan T F.Lithosphere tectonic detachment,magmatism and earthquake in Eastern China of Cenozoic[J].Geoscience,2008,22(2):199-221(in Chinese).
[161]Wan T F.Crust rotation in Jurassic and transformation of lithosphere of Eastern China[J].Geological Bulletin of Chi-na,2004,23(9-10):969-972(in Chinese).
[162]Zhou X H.Major transformation of subcontinental litho-sphere beneath Eastern China in the Cenozoic-Mesozoic:re-view and prospect[J].Earth Science Frontiers,2006,13(2):50-64(in Chinese).
[163]Deng J F,Zhao H L,Wu Z X,et al.A mantle plume be-neath the north part of China continent and lithosphere mo-tion[J].Geoscience,1992,6(3):267-274(in Chinese).
[164]Deng J F,Zhao H L,Mo X X,et al.Continental roots-plume tectonics of China—key to the continental dynamics[M].Beijing:Geological Publishing House,1996:1-105(in Chinese).
[165]Lu F X,Zheng J P,Li WP,et al.The main evolution pat-tern of Phanerozoic mantleinthe Eastern China:the“mush-roomcloud”model[J].Earth Science Frontiers,2000,7(1):97-107(in Chinese).
[166]Zhou X M,Li WX.Origin of Late Mesozoic igneous rocks in southeastern China:i mplications for lithosphere subduc-tion and underplating of mafic magmas[J].Tectonophysics,2000,326(3-4):269-287.
[1]万天丰.中国大地构造学纲要[M].北京:地质出版社,2004:1-387.
[2]滕吉文,曾融生,闫雅芬.东亚大陆及周边海域Moho界面深度分布和基本格局[J].中国科学:D辑,2002,32(2):89-100.
[3]刘光鼎.中国大陆构造格架的动力学演化[J].地学前缘,2007,14(3):39-46.
[4]蔡学林,朱介寿,曹家敏,等.东亚西太平洋巨型裂谷体系岩石圈与软流圈结构及动力学[J].中国地质,2002,29(3):234-245.
[5]朱介寿.欧亚大陆及边缘海岩石圈的结构特性[J].地学前缘,2007,14(3):1-20.
[6]路凤香,吴其反.中国东部典型地区下部岩石圈组成、结构和层圈相互作用[M].武汉:中国地质大学出版社,2005:1-195.
[7]石油地质志编写组.大庆油田[M]∥翟光明.石油地质志,卷二(上).北京:石油工业出版社,1993:34-40.
[8]王凯红,裴福萍,冯玉生,等.延边明月沟盆地中生代火山岩深源捕虏体和捕虏晶的发现及矿物化学[J].吉林地质,2005,24(2):21-27.
[9]赵全国,许文良,靳克,等.延边地区中生代火山岩的岩浆源区:来自Sr-Nd同位素和深源捕虏体(晶)的证据[J].吉林大学学报:地球科学版,2005,35(4):416-422.
[10]孙德有,吴福元,林强,等.张广才岭燕山早期白石山岩体成因与壳幔相互作用[J].岩石学报,2001,17(2):227-235.
[11]林强,葛文春,吴福元,等.大兴安岭中生代花岗岩类的地球化学[J].岩石学报,2004,20(3):403-412.
[12]尹志刚,张跃龙,杨晓平,等.大兴安岭北部中生代火山岩特征及岩浆演化[J].世界地质,2006,25(2):120-128.
[13]薛钢,骆剑英,刘金玉.大兴安岭中南段中生代火山岩特征及成因[J].内蒙古科技与经济,2006,4:100-102.
[14]肖成东,张忠良,赵利青.东蒙地区燕山期花岗岩Nd、Sr、Pb同位素及其岩石成因[J].中国地质,2004,31(1):57-63.
[15]陈义贤,陈文寄,周新华,等.辽西及邻区中生代火山岩[M].北京:地震出版社,1997.
[16]邵济安,翟明国,张履桥,等.晋冀蒙交界地区五期岩墙群的界定及其构造意义[J].地质学报,2005,79(1):56-67.
[17]洪大卫,王涛,童英.华北地台和秦岭—大别—苏鲁造山带的中生代花岗岩与深部地球动力学过程[J].地学前缘,2003,10(3):231-256.
[18]阎国翰,许保良,牟保磊,等.太行山—大兴安岭东麓碱性侵入岩年代学和锶、钕、铅同位素特征及其意义[J].地质学报,2000,74(4):774-781.
[19]魏俊浩,刘丛强,唐红峰.辽东五龙地区燕山期侵入岩类同源岩浆演化微量元素、同位素证据与金矿成矿[J].地质论评,2003,49(3):265-271.
[20]张旗,赵太平,王焰,等.中国东部燕山期岩浆活动的几个问题[J].岩石矿物学杂志,2001,20(3):273-280,292.
[21]姜耀辉,蒋少涌,赵葵东,等.辽东半岛煌斑岩SHRI MP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约[J].科学通报,2005,50(19):2161-2168.
[22]汪洋,邓晋福.冀晋辽地区燕山期强过铝质侵入岩岩石化学特征及其动力学意义[J].地质通报,2002,21(4-5):270-276.
[23]吴利仁.华东及邻区中、新生代火山岩[M].北京:科学出版社,1984.
[24]陈志宏,陆松年,李怀坤,等.秦岭造山带富水中基性侵入杂岩的成岩时代——锆石U-Pb及全岩Sm、Nd同位素年代学新证据[J].地质通报,2004,23(4):322-328.
[25]张宏,袁洪林,胡兆初,等.冀北滦平地区中生代火山岩中单颗粒锆石的稀土元素特征及启示[J].中国稀土学报,2006,24(2):227-234.
[26]许文良,林景仟.河北邯邢地区角闪闪长岩中地幔纯橄岩包体的发现与研究[J].地质学报,1991,65(1):33-41.
[27]李伍平,李献华.燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义[J].岩石学报,2004,20(3):247-254.
[28]牛树银,陈路,许传诗,等.太行山区地壳演化及成矿规律[M].北京:地震出版社,1994:1-203.
[29]万天丰,Teyssier C,曾华霖,等.山东玲珑花岗质岩体侵位机制[J].中国科学:D辑,2000,30(4):337-344.
[30]罗振宽,苗来成.胶东招莱地区花岗岩和金矿床[M].北京:冶金工业出版社,2002:20-57.
[31]郭敬辉,陈福坤,张晓曼,等.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞-碰撞后构造过程:锆石U-Pb年代学[J].岩石学报,2005,21(4):1281-1301.
[32]孙丰月.胶东地区中新生代区域构造演化与成矿[J].长春地质学院学报,1994,24(4):378-384.
[33]陈光远,孙岱生,周若,等.胶东郭家岭花岗闪长岩成因矿物学与金矿化[M].武汉:中国地质大学出版社,1993:1-230.
[34]石油地质志编写组.胜利油田[M]∥翟光明.石油地质志,卷六.北京:石油工业出版社,1993:264-271.
[35]曾键年,左大华,马宪.山西塔儿山地区燕山期岩浆演化及其对金属成矿的控制作用[J].华北地质矿产杂志,1997,12(1):33-43.
[36]真允庆.五台山—恒山一带金、银多金属矿床同位素地球化学及其成矿模型[J].桂林工学院学报,2004,24(2):127-136.
[37]山西地质矿产局.山西省区域地质志[M].北京:地质出版社,1989:1-780.
[38]李曙光,黄方,李晖.大别—苏鲁造山带碰撞后的岩石圈拆离[J].科学通报,2001,46(17):1487-1491.
[39]管运才,吴海权.白马尖超单元组合特征及其成因机制[J].安徽地质,1997,7(2):26-35.
[40]南京大学地质学系.华南不同时代花岗岩类及其与成矿关系[M].北京:科学出版社,1981.
[41]杜杨松,秦新龙,李铉具.安徽铜陵地区中生代幔源岩浆底侵作用——来自矿物巨晶和岩石包体的证据[J].岩石矿物学杂志,2004,23(2):109-116.
[42]王元龙,王焰,张旗.铜陵地区中生代中酸性侵入岩的地球化学特征及其成矿-地球动力学意义[J].岩石学报,2004,20(2):325-338.
[43]楼亚儿,杜杨松.安徽繁昌—铜陵中生代侵入岩的黑云母特征和成因探讨[J].矿物学报,2006,26(2):175-180.
[44]王彦斌,刘敦一,曾普胜,等.安徽铜陵地区幔源岩浆底侵作用的时代——朝山辉石闪长岩锆石SHRI MP定年[J].地球学报,2004,25(4):423-427.
[45]许文良,王清海,王冬燕,等.华北克拉通东部中生代岩石圈减薄的过程与机制:中生代火成岩河深源捕虏体证据[J].地学前缘,2004,11(3):309-317.
[46]翟裕生,姚书振,周若,等.长江中下游铁铜(金)成矿规律[M].北京:地质出版社,1992:1-235.
[47]周泰禧,陈江峰,李学明,等.安徽省印支期岩浆活动质疑[J].岩石学报,1988(3):46-53.
[48]王德滋,周新民,舒良树,等.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化[M].北京:科学出版社,2002.
[49]李永军,谢其山,孪新东,等.西秦岭糜署岭岩浆带成因及构造意义[J].新疆地质,2004,22(4):374-377.
[50]刘埃平,金景福.牧护关花岗岩中锆石标型特征研究[J].地质地球化学,1996,4:15-20.
[51]尚瑞钧,严阵,黄云玉,等.秦巴花岗岩[M].武汉:中国地质大学出版社,1988.
[52]胡海珠,李毅.豫西熊耳山地区燕山期岩浆作用对金银成矿的制约因素[J].矿产与地质,2006,20(4-5):427-429.
[53]严阵,许全成,张海军,等.陕西省花岗岩[M].西安:西安交通大学出版社,1985.
[54]杨起,吴冲龙,汤达祯,等.中国煤变质作用[M].北京:煤炭工业出版社,1996:1-212.
[55]朱介寿,蔡学林,曹家敏,等.中国华南及东海地区岩石圈三维结构及演化[M].北京:地质出版社,2005:1-308.
[56]高天钧,王振民,吴克隆,等.台湾海峡及其周边地区构造岩浆演化与成矿作用[M].北京:地质出版社,1999:1-203.
[57]李向前,陈炯达,潘明宝,等.江苏赣榆城头地区中生代侵入岩石谱系单位划分[J].江苏地质,1999(2):80-83.
[58]周若,杨静,任进.苏州地区I-A型花岗岩特征与成因的对比研究[J].地球科学,1997,22(3):240-246.
[59]周涛发,袁峰,侯明金,等.江南隆起带东段皖赣相邻区燕山期花岗岩类的成因及形成的地球动力学背景[J].矿物岩石,2004,24(3):65-71.
[60]蒋国豪,胡瑞忠,谢桂青,等.大吉山花岗岩体黑云母地球化学特征及其成岩成矿意义[J].矿物岩石,2005,25(5):58-61.
[61]陈培荣,华仁民,章邦桐,等.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学:D辑,2002,45(8):755-768
[63]陈小明,陆建军,刘昌实,等.桐庐、相山火山-侵入杂岩单颗粒锆石U-Pb年龄[J].岩石学报,1999,15(2):272-278.
[64]凌洪飞,沈渭洲,黄小龙.福建省花岗岩类Nd-Sr同位素特征及其意义[J].岩石学报,1999,15(2):255-262.
[65]罗小洪.九瑞地区中生代岩浆活动及其大地构造意义[J].东华理工学院学报,2006,29(2):121-126.
[66]余心起,舒良树,邓国辉,等.江西吉泰盆地碱性玄武岩的地球化学特征及其构造意义[J].现代地质,2005,19:133-140.
[67]赖章忠,王安诚.赣南中生代火山活动时代及岩浆来源[J].江西地质,1996,10:111-118.
[68]周金城,蒋少涌,王孝磊,等.华南中侏罗世玄武岩的岩石地球化学研究——以福建藩坑玄武岩为例[J].中国科学:D辑,2005,35(10):927-936.
[69]江剑丽.福建晚侏罗世两条性质不同的巨型火山岩带[J].福建地质,2001,20(4):171-176.
[70]张文兰,华仁民,王汝成,等.赣南大吉山花岗岩成岩与钨矿成矿年龄的研究[J].地质学报,2006,80(7):956-962.
[71]吴广宇.广宁花岗岩质杂岩的地质年代学研究[J].广东地质,1986,1:1-22.
[72]叶伯丹.两广云开地区同位素年龄数据及其地质意义[J].广东地质,1989,3:39-55.
[73]崔遥.河台花岗岩同位素地质年代学及成因演化[C]∥第四届全国同位素会议论文(摘要)汇编,1989:58-59.
[74]王联魁,沙连埅,徐文新,等.论花岗岩建造与系列——兼论花岗岩三级成因分类[M].广州:广东科技出版社,2003.
[75]耿红燕,徐夕生,O Reilly S Y,等.粤西白垩纪火山-侵入岩浆活动及其地质意义[J].中国科学:D辑,2006,36(7):601-617.
[76]华仁民.南岭中生代陆壳重熔型花岗岩类成岩-成矿的时间差及其地质意义[J].地质论评,2005,51(6):27-33.
[77]张树明,巫建华,周维勋,等.南岭东段燕山期镁铁质岩石Nd-Sr同位素研究[J].东华理工学院学报,2004,27(2):129-135.
[78]马铁球,邝军,柏道远,等.南岭中段诸广山南体燕山早期花岗岩地球化学特征及其形成的构造环境分析[J].中国地质,2006,33(1):119-131.
[79]陈培荣,周新民,张文兰,等.南岭东段燕山早期正长岩-花岗岩杂岩的成因和意义[J].中国科学:D辑,2004,34(6):493-503.
[81]付建明,马昌前,谢才富,等.湖南金鸡岭铝质A型花岗岩的厘定及构造环境分析[J].地球化学,2005,34(3):215-226.
[83]孔华,马芳,黄德志.湖南地区深部岩石剖面的建立——来自深源岩石包体的证据[J].桂林工学院学报,2001,21(3):195-201.
[84]陈必河,贾宝华,刘耀荣,等.湘南中生代火山岩中尖晶石二辉橄榄岩包体Sm-Nd等时线年龄及地质意义[J].地质论评,2004(2):180-183.
[85]顾晟彦,华仁民,戚华文.广西姑婆山花岗岩单颗粒锆石LA-ICP-MS U-Pb定年及全岩Sr-Nd同位素研究[J].地质学报,2006,80(4):543-553.
[86]郭新生,陈江峰,张巽,等.桂东南富钾岩浆杂岩的Nd同位素组成:华南中生代地幔物质上涌事件[J].岩石学报,2001,17(1):19-27.
[87]王建辉,蒋柏昌,孔祥伟,等.姑婆山复式岩体的基本特征及其与成矿作用的关系[J].矿产与地质,2006,20(1):47-53.
[88]曾华霖,刘军,张庆合.华南地区重磁资料处理解释及其在华南地壳结构研究中的应用[M]∥岩石圈构造与动力学开放研究实验室,1994年年报.北京:地震出版社,1995:87-101.
[89]战明国.华南中生代构造-岩浆-成矿作用及区域成矿规律研究[D].宜昌:中国地质科学院宜昌地质矿产研究所,1994.
[90]陈祥,肖力.内蒙古额仁陶勒盖银矿床地球化学研究[J].贵金属地质,1999,8(3):171-178.
[91]邵济安,贾文,储著银等.内蒙古喀喇沁早白垩世橄辉云煌岩岩筒[J].岩石学报,2003,19(3):429-434.
[92]张宏福,郑建平.华北中生代玄武岩的地球化学特征与岩石成因——以辽宁阜新为例[J].科学通报,2003,48(6):603-609.
[94]路凤香,朱勤文,谢意红,等.英安岩中高压辉石巨晶的发现及其意义[J].地球科学——中国地质大学学报,1996,21(5):541-544.
[95]张辉煌,徐义刚,葛文春,等.吉林伊通—大屯地区晚中生代-新生代玄武岩的地球化学特征及其意义[J].岩石学报2006,22(6):1579-1596.
[96]刘若新,陈文寄,解广轰,等.中国新生代火山岩年代学与地球化学[M].北京:地震出版社,1992.
[97]张星.吉林省四平山门早白垩世流纹岩地质特征[J].吉林地质,2001,20(3):30-34.
[98]郑常青,许文良,王冬艳.辽西阜新中生代玄武岩中深源捕虏体的岩石学和矿物化学研究[J].岩石学报,1999,15(4):616-622.
[99]邵济安,李之彤,张履桥.辽西及邻区中-新生代火山岩的时空对称分布及其启示[J].地质科学,2004,39(1):98-106.
[100]张招崇,李兆鼐,王富宝,等.辽西义县盆地火山岩的基本特征及其成因探讨[J].现代地质,1994,8(4):441-451.
[101]邵济安,张履桥,魏春景,等.北京南口中生代双峰式岩墙群的组成及其特征[J].地质学报,2001,75(2):205-212.
[102]苏尚国,邓晋福,赵国春.北京燕山地区薛家石梁杂岩体特征、成因、源区性质及岩石圈减薄方式[J].地学前缘,2006,13(2):148-157.
[103]蔡剑辉,阎国翰,牟保磊,等.北京房山岩体锆石U-Pb年龄和Sr、Nd、Pb同位素与微量元素特征及成因探讨[J].岩石学报,2005,21(3):776-788.
[104]邵济安,李献华,张履桥,等.南口—古崖居中生代双峰式岩墙群形成机制的地球化学制约[J].地球化学,2001,30(6):517-524.
[105]石油地质志编写组.大港油田[M]∥翟光明.石油地质志,卷四.北京:石油工业出版社,1991:92-95.
[106]陈斌,刘超群,田伟.太行山中生代岩浆作用过程中的壳幔岩浆混合作用:岩石学和地球化学证据[J].地学前缘,2006,13(2):140-147.
[107]张勇,陈斌,邵济安,等.华北太行晚中生代煌斑岩地球化学特征及成因探讨[J].岩石矿物学杂志,2003,22(1):29-33.
[108]孟繁聪,李天福,薛怀民,等.胶莱盆地晚白垩世不同地幔源区的两种基性岩浆——诸城玄武岩和胶州玄武岩的对比[J].岩石学报,2006,22(6):1644-1656.
[109]闫峻,陈江峰,谢智,等.鲁东晚白垩世玄武岩及其中幔源包体的岩石学和地球化学研究[J].岩石学报,2005,21(1):99-110.
[112]闫峻,陈江峰,榭智,等.鲁东晚白垩世玄武岩中的幔源捕虏体:对中国东部岩石圈减薄时间制约的新证据[J].科学通报,2003,48(14):1570-1574.
[113]刘晓煌,王金荣,孙兴丽,等.招掖金矿区带花岗岩与金成矿作用研究[J].有色金属,2006,58(4):15-20.
[114]裴福萍.鲁西费县中生代玄武岩及幔源捕掳晶的矿物化学:对岩石圈地幔性质的制约[J].高校地质学报,2004,10(1):88-97.
[115]王冬艳,许文良,兰翔,等.鲁西中生代辉长闪长岩中辉石岩捕虏体的岩石成因[J].吉林大学学报:地球科学版,2004,34(2):167-173.
[116]万天丰.山东省构造演化和应力场研究[J].山东地质,1992,8(2):70-101.
[117]李晓勇,范立勇.西秦岭地区晚中生代OIB型玄武岩的发现及其意义[J].中山大学学报:自然科学版,2006,45(3):127-128.
[118]李家振,张爱民.北淮阳金寨—苏仙石地区中生代花岗岩的成因类型及岩浆演化特征[J].现代地质,1997,11(2):253-260.
[119]李曙光,黄方,李晖.大别—苏鲁造山带碰撞后的岩石圈拆离[J].科学通报,2001,46(17):1487-1491.
[120]王强,赵振华,简平,等.华南腹地白垩纪A型花岗岩类或碱性侵入岩年代学及其对华南晚中生代构造演化的制约[J].岩石学报,2005,21(3):795-808.
[121]马昌前,杨坤光,许长海,等.大别山中生代钾质岩浆作用与超高压变质地体的剥露机理[J].岩石学报,1999,15(3):379-395.
[122]翟建平.昆山、城山和大龙山岩体的锶同位素特征及其成因研究[J].地球化学,1989,3:202-209.
[123]张德全,徐洪林.长江中下游花岗岩类地质地球化学对比研究[J].华南地质与矿产,2002,3:66-77.
[124]邢凤鸣,徐祥.安徽两条A型花岗岩带[J].岩石学报,1994,10(4):357-369.
[125]邢凤鸣.安徽沿江地区中生代岩浆的基本特点[J].岩石学报,1995,11(4):409-422.
[126]李文达,毛建仁,朱云鹤,等.中国东南部中生代火成岩与矿床[M].北京:地震出版社,1998.
[127]邢凤鸣,徐祥.安徽扬子岩浆岩带与成矿[M].合肥:安徽人民出版社,1999:1-170.
[128]靳克,许文良,王清海,等.蚌埠淮光“混合花岗闪长岩”的形成时代及源区:锆石SHRI MP U-Pb地质年代学证据[J].地球学报,2003,24(4):331-335.
[129]杨德彬,许文良,裴福萍,等.蚌埠隆起区花岗岩形成时代及岩浆源区性质:锆石LA-ICPMS U-Pb定年与示踪[J].地球化学,2005,34(5):443-454.
[130]牛漫兰.张八岭隆起南缘早白垩世火山岩稀土元素对比研究[J].中国稀土学报,2006,24(6):739-744.
[131]吴才来,周若,黄许陈,等.安徽茅坦A型花岗岩研究[J].地质学报,1998,72(3):237-247.
[132]章邦桐,张富生,倪琦生,等.安庐石英正长岩带的地质和地球化学特征及成因探讨[J].岩石学报,1988,4(3):1-12.
[133]闫峻,陈江峰,谢智,等.长江中下游地区蝌蚪山晚中生代玄武岩的地球化学研究:岩石圈地幔性质与演化的制约[J].地球化学,2005,34(5):455-469.
[134]戚学祥,旷宏伟,陈培良,等.长江中下游燕山期侵入岩地球化学特征及其地质意义[J].资源调查与环境,2002,23(1):52-59.
[136]陈江峰,Foland K A,刘义茂.苏州复式花岗岩体的精确40Ar/39Ar定年[J].岩石学报,1993,9(1):77-85.
[137]叶水泉.江苏宁镇伏牛山岩体的铷锶等时线年龄[J].江苏地质,1999,23(3):148-150.
[138]龚新法,管建强.浙东南楠溪江中下游地区火山岩地质特征及演化规律[J].浙江地质,1998,14(1):11-17.
[139]陈江峰.简单混合、AFC混合花岗岩同位素数据解释[J].安徽地质,1991,1:19-27.
[140]王中杰,杨琴芳,阮宏宏,等.浙闽赣中生代火山岩地质若干基本问题[J].中国地质科学院南京地质矿产研究所所刊,1987,8(3):1-14.
[141]邱检生,王德滋,McInnes B I A.浙闽沿海地区I型-A型复合花岗岩体的地球化学及成因[J].岩石学报,1999,15(2):237-246
[142]洪大卫,谢锡林,张季生.试析杭州—诸广山—花山高εNd值花岗岩带的地质意义[J].地质通报,2002,21(6):348-354.
[143]周金城,张海进,俞云文.浙江新昌早白垩世复合岩流中岩浆混合作用[J].岩石学报,1994,10(3):236-247.
[144]黄泉祯.1∶500000福建省区域地质图说明书[M].福州:福建地图出版社,1998:1-120.
[145]邱检生,王德滋,McInnes BI.福建沿海铝质A型花岗岩的地球化学及岩石成因[J].地球化学,2000,29(4):313-321.
[146]邱检生,王德滋,周金城.福建永泰云山晚中生代双峰式火山岩的地球化学及岩石成因[J].岩石矿物学杂志,1999,18(2):97-107.
[147]张德全,佘宏全,阎开好,等.福建紫金山地区中生代构造环境转换的岩浆岩地球化学证据[J].地质论评,2001,47(6):608-616.
[148]洪大卫,郭文岐,李戈晶,等.福建沿海晶洞花岗岩带的岩石学和成因演化[M].北京:北京科学技术出版社,1987.
[149]毛建仁,陶奎元,李寄嵎,等.闽西南地区中生代花岗闪长质岩石的特征及其构造演化[J].岩石矿物学杂志,2002,21(2):135-142.
[150]周若,吴克隆.漳州I-A型花岗岩[M].北京:科学出版社,1994.
[151]廖群安,王京名,薛重生,等.江西广丰白垩系盆地中两类玄武岩的特征及其与盆地演化的关系[J].岩石学报,1999,15(1):116-123.
[152]王勇,余达淦.赣东北早白垩世中酸性火山-侵入杂岩微量元素地球化学特征及成因探讨[J].江西地质,2000,14(4):251-255.
[153]余心起,舒良树,颜铁增,等.江山—广丰地区早白垩世晚期玄武岩的岩石地球化学及其构造意义[J].地球化学,2004,33(5):465-474.
[154]王祖伟,周永章,张海华,等.粤西庞西垌银矿床稀土元素地球化学[J].黄金地质,1999,5(2):52-54.
[155]张宗胜.白云嶂中生代晚期碱性火山岩的基本特征与成岩构造环境[J].广东地质,2001,16(4):22-28.
[156]徐夕生,周新民,Reillysy O,等.中国东南下地壳物质与花岗岩成因探索[J].岩石学报,1999,15(2):217-223.
[157]贾大成,胡瑞忠,卢焱.湘东南汝城盆地火山岩的元素地球化学及源区性质讨论[J].现代地质,2003,17(2):131-136.
[158]许德如,贺转利,李鹏春,等.湘东北地区晚燕山期细碧质玄武岩的发现及地质意义[J].地质科学,2006,41(2):311-332.
[159]彭头平,王岳军,彭冰霞,等.湘东北应家山古近纪玄武岩地球化学特征及其成因意义[J].地球化学,2006,35(4):395-404.
[160]王亚妹,万天丰.中国东部新生代岩石圈构造滑脱、岩浆活动和地震[J].现代地质,2008,22(2):199-221.
[161]万天丰.侏罗纪地壳转动与中国东部岩石圈转型[J].地质通报,2004,23(9-10):969-972.
[162]周新华.中国东部中、新生代岩石圈转型与减薄研究若干问题[J].地学前缘,2006,13(2):50-64.
[163]邓晋福,赵海玲,吴宗絮,等.中国北方大陆下的地幔热柱与岩石圈运动[J].现代地质,1992,6(3):267-274.
[164]邓晋福,赵海玲,莫宣学,等.中国大陆根-柱构造——大陆动力学的钥匙[M].北京:地质出版社,1996:1-105.
[165]路凤香,郑建平,李伍平,等.中国东部显生宙地幔演化的主要样式:“蘑菇云”模型[J].地学前缘,2000,7(1):97-107.
目录