[1] Zindler A. Nd,Sr and Pb isotopic systematics in a three component mantle, a new perspectiv[J].Nature,1982,289:519~523. [2] Dupre B, Allehre C J. Pb-Sr isotope variations in Indian Ocean basalts and mixing phenomena[J].Nature,1983,303:142~146. [3] Hart S R. A large-scale isotope anomaly in the southern hemisphere mantle[J]. Nature,1984,309:753~757. [4] Castillo P R. The Dupal anomaly as a trace of the upwelling lower mantle[J]. Nature,1988,336:667~670. [5] Klein E M,Langmuir C H,Zindler A,et al. Isotope evidence of a mantle convection boundary at the Australian-Antarctic discordance[J].Nature,1988,333:623~628. [6] Mahoney J J, le Roex A P, Peng Z,et al. Southwestern limits of Indian Ocean ridge mantle and the origin of low206Pb/204Pb mid-ocean ridge basalt: isotope systematics of the central Southwest Indian Ridge (17~50°E)[J].J Geophy Res,1992,97:19 771~19 790. [7] Mahoney J J, Frei R. Tejada M L G,et al. Tracing the Indian ocean mantle domain through time:Isotopic results from old west Indian,East Tethyan,and South Pacific seafloor[J].J Petrology,1998, 39:1 285~1 306. [8] Pyle D G,Christie D M, Mahiney J J. Resolving an isotopic boundary within the Australian-Antarctic discordance [J].Earth Planet Sci Lett,1992,112:161~178. [9] Hickey-Vrgas R.Origin of the Indian Ocean-type isotopic signature in basalts from Philippine Sea plate spreading centers:An assessment of local versus large-scale processes[J].J Geophy Res,1998,103(B9):20 963~20 979. [10] Dosso L,Bougaukt H,Langmuir C,et al. The age and distribution of mantle heterogeneity along the mid Atlantic ridge (31~41°N)[J].Earth Planet Sci Lett,1999,170:269~286. [11] Hofmann A W.Origin of the Hawaiian mantle plume[J].China Sci Bull,1998,43(Supp.):52. [12] Humler E,Thirot J L, Montagner J P.Global correlations of mid-ocean-ridge basalts chemistry with seismic tomographic image[J].Nature,1993,364:225~228. [13] Zhu B Q,Mao C X, Lugmair G W,et al.Isotopic and geochemical evidence for the origin of Plio-Pleistocene volcanic rocks near Indo-Eurasian collisional margin at Tengchong, China[J].Earth Planet Sci Lett,1983,65:263~275. [14] Zhu B Q,Li X H, Liu B L. Three-component mixing and four system recycling models for explaining Nd-Sr-Pb isotopic correlation of suboceanic and subcontinental mantles[J].Science in China (B),1990,33:757~768. [15] Zhu B Q, Wang H F. Geochronology of and Nd-Sr-Pb isotopic evidences for mantle source in the ancient subduction zone beneath Sanshui Basin,Guangdong Province,China[J].Chinese J of Geochemistry,1989,8(1):65~71. [16] Zhu B Q.Evidence of isotopic systematics from crust and mantle for chemical heterogeneities of terranes[J].Chinese Science Bulletin,1991,36(15):1 279~1 282. [17] Peng Z C,Zartman R E, Fuda E.et al. Pb-,Sr-,and Nd-iso-topic systematics and chemical characteristics of Cenozoic basalts,Eastern China[J].Chemical Geology,1986,59:3~33. [18] Basu A R,Xie G H, Huang A K,et al.Major element,Ree, and Pb,Nd and Sr isotopic geochemistry of Cenozoic volcanic rocks of eastern China:implications for their origin from suboceanic-type mantle reservoirs [J]. Earth Planet Sci Lett,1991,105:149~169. [19] Zhu Bingquan, Wang Huifen. NdˉSrˉPb isotopic and chemical evidence for the volcanism with MORB-OID source characteristics in the Leiqiong area[J].China,Geochimica,1989, (3):193~201.[朱炳泉,王慧芬.雷琼地区MORB-OIB过渡型地幔源的Nd-Sr-Pb同位素证据[J].地球化学,1989,(3):193~201.] [20] Zhu Bingquan,Zhang Yuquan, Xie Yingwen.Nd,St and Pb isotopic characteristics of Cenozoic ultraˉpotassic volcanic rocks from eastern Erhai,Yunnan and their implications for subcontinent mantle evolution in southwestern China [J].Geochimica,1992,(3):201~212.[朱炳泉,张玉泉,谢应雯.滇西洱海第三纪超钾质火成岩系的Nd-Sr-Pb同位素特征与西南大陆地幔演化[J].地球化学,1992,(3):201~212.] [21] Zhu Bingquan,Wang Huifen,Zou Liping,et al.Discussion on mantle geochemistry and division of Cathaysian-Yangtze mantle boundary in Zhe jiang-Fuzhou areas.In: Li Jiliang.Beijing:Metallurgic Industry Press,1993.60~68.[朱炳泉,王慧芬,邹丽萍,等.浙闽地幔地球化学与华南—扬子地幔边界划分讨论[A].见:李继亮主编.东南大陆岩石圈结构与地质演化[C].北京:冶金工业出版社,1993.60~68.] [22] Liu Beiling, Chen Yuwei, Zhu Bingquan.Genesis of Cenozoic basalts in Jinbo Lake,N-E China,and its chemical feature of mantle,Nd,Sr,Pb isotopic and trace elemental evidence[J].Geochimica,1989,(1):9~19.[刘北玲,陈毓蔚,朱炳泉.东北镜泊湖新生代玄武岩的成因及其地幔化学特征——Sr、Nd、Pb同位素与微量元素证据[J].地球化学,1989,(1):9~19.] [23] Zhang Benren,Lao T C,Gao S.Geochemical study of the lithosphere, tectonism and metallogenesis in the Qinling-Dabashan region [M]. Wuhan: China Univ Geosci Press,1994. [张本仁等.秦巴岩石圈构造及成矿规律地球化学研究[M].武汉:中国地质大学出版社,1994.] [24] Zhang Benren,Zhang Hongfei,Zhao Zhidan,et al.Geochemical subdivision and evoltuion of lithosphere in East Qinling and adjacent regions-Implication for tectonics[J].Science in china(D),1996,39(3):245~255.[张本仁,张宏飞,赵志丹,等.东秦岭及邻区壳、幔地球化学分区演化及其大地构造意义[J].中国科学(D),1996,26(3):201~208.] [25] Yu J, Gui X. Isotope geochemistry of granitoids[A]. In: Tu G,Chow T. Isotope Geochemistry Research in China[C].Beijing: Science Press,1998.137~161. [26] Li Shi,Wang Dang.Geochemistry of Granitoids in Tongbais-han-Dabishan,Central China[M].Wuhan:China Univ Geosci Press,1991.[李石,王丹.桐柏山—大别山花岗类地球化学[M].武汉:中国地质大学出版社,1991.] [27] Zhang Ligang,et al.Block Geology of Eastern Asia Lithosphere[M].Beijing:Science Press,1995.[张理刚等.东南岩石圈块体地质[M].北京:科学出版社,1995.] [28] Zhu B Q.Geochemical evidences for the southern China block being a part of Gondwana[J].J S Asian Earth Sci,1994,9:319~324. [29] Zhu Bingquan.The mapping of geochemical provinces in China based on Pb isotopes[J].J Geochem Exploration,1995,55:171~181. [30] Zhu Bingquan. Tri-dimension spatial topological diagrams of ore lead isotopes and their application to the division of geochemical provinces and mineralizations[J].Geochimica,1993,(3):210~216.[朱炳泉.矿石Pb同位素三维空间拓扑图解用于地球化学省与矿种区划[J].地球化学,1991,(3):210~216.] [31] Yin A, Harrison T M. Geologic evolution of the Himalayan-Tibetan orogen[J]. Ann Rev Earth Planet Sci, 2000, (in press). [32] Sengor A M. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J].Nature,1993,364:298~306. [33] Wang Qianshen,Wu Chuanzhen,Liu Hongchen,et al.Discussion on distribution pattern of orustal thickness and crustal structure of Asian continent[J].Seismic Geology,1982,4(3):1~9.[王谦身,武传真,刘洪臣,等.亚洲大陆地壳厚度分布轮廓及地壳构造特征的探讨[J].地震地质,1982,4(3):1~9.] [34] Liu Guangding.Discussion on Earth Sciences[J].Earth Science Frontiers,1998,5(1) 1~8.[刘光鼎.论地球科学[J].地学前缘,1998,5(1):1~8.] [35] Yuan Xuecheng.Velocity structure of the Qinling lithosphere and mushroom cloud model[J].Science in China(D),39(3):235~244.[袁学诚.秦岭岩石圈速度结构与蘑菇云构造模型[J].中国科学(D),1996,26(3):209~215.] [36] Xiong Shaobai, Lai Minghui,Liu Hongbin,et al.Lithosphere structure and velocity distribution in Tunxi-Wenzhou areas[A].In:Li Jiliang. Beijing:Metallurgic Industry Press,1993.250~256.[熊绍柏,赖明惠,刘宏宾,等.屯溪—温州地带的岩石圈结构与速度分布[A].见:李继亮主编.东南大陆岩石圈结构与地质演化[C].北京:冶金工业出版社,1993.250~256.] [37] Yan Yafen,Ren Guotai,Zheng shuanggen.The relationship between geomagnetic field feature and crustal structure for lithosphere in Southeast China[A].In:Li Jianged.BeijingL-Metallurgic Industry Press,1993,238~241.[闫雅芬,任国泰,郑双根.东南大陆岩石圈的地磁区域场特征与地壳结构的关系[A].见:李继亮主编.东南大陆岩石圈结构与演化[C].北京:冶金出版社,1993.238~241.] [38] Jin Wenshan, Sun Dazhong. Deep crustal structure of South China continent and its evolution [M]. Beijing: Geological Press,1996.[金文山,孙大中.华南大陆深部地壳结构及其演化[M].北京:地质出版社,1993.] [39] Wang Maoji.Gravity and geomzagnetic illustration of Heshan-Quanzhou profile[J].Geophysics Acta,1994,37(3):321~329.[王懋基.黑山—泉州地学断面的重磁解释[J].地球物理学报,1994,37(3):321~329.] [40] Zhu B-Q, Dong Y-P, Chang X-Y,et al.Relation of isotopic geochemical steep zones with geophysical fields tectonics in the junction area of the Cathaysian, Yangtze and Indochia plates[J].Acta Geol Sinica,2000,74(2):236~240. [41] Zhao Yonggui,Zhong Dalai, Liu Jianhua,et al.Principle of geological illustration of seismic tomography and its application to study on deep structure in western Yunnan[J].Geological Science,1992,(2):105~113.[赵永贵,钟大赍,刘建华,等.地震层析地质解释原理及其在滇西深部构造研究中的应用[J].地质科学,1992,(2):105~113.] [42] Zhu B Q.Discussion on geochemical division and affinity of East Asia blocks:Implications for tectonic framework[A].In: Metcalfe I,ed.Gondwana Dispersion and Asian Accretion-Final Result of IUGS IGCP 321[C].Netherland,A A Balkema Pub,1998.211~227. [43] Dong Y P, Zhu B Q,Chang X Y.Tectonic implications of the isotopic geochemical steep zone in eastern Yunnan,China[J].Chinese Sci Bull,1999,44(Supp.2):195~196. [44] Dong Y P, Zhu B Q.Characteristics of the island—Arc pillow lavas from sortheast Yunnan Province,and its tectonic implications for paleo-tethys in south China[J].Chinese Sci Bull,2000,45(8):753~758. [45] Zhu B Q,Chang S Y,Wang H F. The geochemical boundary between South China and Yangtze blocks and its constraint on the formation of super large deposits[J].Science in China(D),1996,39(1):58~65. [46] Zhu B Q,Chang X Y, Qiu H N,et al.Characteristics of Proterozoic basements on the geochemical steep zones in the continent of China and their implications for setting of super large deposits[J]. Science in China (D),1998,41(Supp.):54~64. [47] Zhang Z W, Zhu B Q,Cai K Q,et al. Lead isotopic steepdipping zone and mineralization—An example from mineral deposits contracted area in East Oinling China[J]. J China Univ Geosci,2000,11(1):287~294. [48] Chang X Y, Zhu B-Q. Lead isotopic exploration intersecting mineralization zones for the depth forecast of concealed deposits—A case from Longbohe Cu deposit,Jinping,Yunnan Province, China[J].Science in China(D),2000,43(1):(in press). [49] Chang Xiangyang,Zhu Bingquan,Sun Dazhong,et al.Isotope geochemistry study of Donghuan copper deposits in Middle Yunnan Province,SW China:I.Stratigraphic chronology and application of geochemical exploration by lead isotopes[J].Geochimica,1997,26(2):32~38.[常向阳,朱炳泉,孙大中,等.东川铜矿同位素地球化学研究:I.地层年代与铅同位素化探应用[J].地球化学,1997,26(2):32~38.] [50] Zhu Bingquan,Zhang Jinglian.A study on distribution regularities of large-and medium size oil and gas fields in China mainland[J].Petroleum Explorationist,1999,4(1):12~17.[朱炳泉,张景廉.中国大陆大中型油气田分布规律探讨[J].勘探家,1999,4(1):12~17.] |