Anderson D L. 1985. Hotspot magmas can form by fractionation and contamination of mid-ocean ridge basalts. Nature, 318:145 ~149.
[3]
Armstrong R L. 1968. A model for Sr and Pb isotope evolution in a dynamic earth. Rev. Geophy. , 6:175 ~ 199.
[4]
Bowring S A, Housh T. 1995. The Earth\'s early evolution. Science,269:1535~1540.
[5]
Condie K C. 1998. Episodic continental growth and supercontinents: a mantle avalanche connection? Earth Planet Sci. Lett., 163: 97~108.
[6]
Condie K C. 2000. Episodic continental growth models: aferthoughts and extensions. Tectonophysics, 322: 153 ~ 162.
[7]
Dobretsov N L, Berzin N A, Buslov M M. 1995. Opening and tectonic evolution of the Paleo-Asian ocean. International Geol.Rev. , 37: 335~360.
[8]
Engebreston D C, Kelley K P, Cashman H J, Richards M A. 1992.180 million years of subduction. GSA Today, 2: 93~95, 100.
[9]
Grand S P, van der Hilst R D, Widiyantoro S. 1997. Global seismic tomography: a snapshot of convection in the earth. GSA, today,7(4) :1~7.
[10]
Hart S R. 1984. A large-scale isotope anomaly in the Southern Hemisphere mantle. Nature, 309: 753~757.
[11]
Hoffman P F. 1989. Speculations on Laurentia\'s first gigayear (2.0 to 1.0Ga). Geology, 17:135~138.
[12]
Hoffman P F. 1992. Supercontinents,in Encyclopedia of Earth system science. Academic, Sandiego, Calf. , 4: 323~328.
[13]
Hong Dawei, Wang Shiguang, Xie Xinlin, Zhang Jisheng. 2000.Genesis of positive εNd granitoids in the Da Hinggar Mts-Mongolia orogenic belt and continental crustal growth. Earth Science Frontiers, 7: 441~456 (in Chinese with English abtracts).
[14]
Hong Dawei, Wang Shiguang, Xie Xilin, Zhang Jisheng. 2001. The Phanerozoic continental growth in central Asia and the evolution of Laurasia supercontinent. Gondawana Res. , 4: 632~633.
[15]
Jahn B M, Wu F, Chen B. 2000b. Masssive granitoid generation in central Asia: Nd isotopic evidence and implication for continental growth in the Phanerozoic. Episodes, 23: 82~92.
[16]
Khain E V, Bibikova E V, Kroner A, Zhuralev D Z, Sklyarov E V, Fedotova A A, Kravchenko-Berezhnoy I R. 2002. The most ancient ophiolite of the Central Asian fold belt: U-Pb and Pb-Pb zircon ages for the Dunzhugur Comples, Eastern Sayan, Siberia, and geodynamic implications. Earth Planet. Sci. Lett. , 199:311~325.
[17]
Larson R L. 1991. Latest pulse of Earth: evidence for a midCretaceous superplume. Geology, 19: 547~550.
[18]
Maruyama S. 1994. Plume tectonics. J. Geod. Soc. Japan, 100(1):24~49.
[19]
McCulloch M T, Chappell B W. 1982. Nd isotopic characteristics of S- and I-type granites. Earth Planet. Sci. Lett. , 58: 51~64.
[20]
Nance R D, Worsley T R, Moody J B. 1988. The supercontinent cycle. Sci. Amer. 256(July): 72~79.
[21]
Peltier W R, Butler S P, Solheim L P. 1997. The influence of phase transformations on mantle mixing and plate tectonics. In: Crossley D J, ed. Earth\'s Deep Interier. Ansterdam: Gordon and Breach,405~430.
[22]
Taylor S R, McLennan S M. 1995. The geochemical evolution of the continental crust. Rev. Geophys. , 33:241~265.
[23]
van der Hilst R D, Karason H. 1999. Compositional heterogeneity in the bottom 1000 kilometers of earth\'s mantle: toward a hybrid convection model. Science, 283:1885~ 1888.
[24]
Albarede F. 1998. The growth of continental crust. Tectonophysics,296:1~14.
[25]
Boher M, Abouchami W, Michard A, Albarede J, Arndt N T. 1992.Crustal growth in West-Africa at 2.1 Ga. J. Geophys. Res. , 97:345~369.
[26]
Breuer D, Spohn T. 1995. Possible flush instability in mantle convection at the Archean-Peoterozoic transition. Nature, 378:608~610.
[27]
Defant M J, Drummond M S. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347:662~665.
[28]
Dupre B, Allegre C. 1983. Pb-Sr isotope variation in Indian Ocean basalts and mixing phenomena. Nature, 303: 142~146.
[29]
Fukao Y, Maruyama S, Obayashi M, Inoue H. 1994. Geologic implication of the whole mantle P-wave tomography. J. Geol. Soc.Japan, 100(1): 4~23.
[30]
Gurnis M. 1988. Large scale mantle convection and aggregation and dispersal of supercontinents. Nature, 332 : 695~699.
[31]
Hawkesworth C J, Mantovani M S M, Taylor P N, Palacz Z. 1986.Evidence from the Parana of south Brazil for a continental contribution to Dupal Basalts. Nature, 322: 356~358.
[32]
Hurley P M, Rand J R. 1969. Pre-drift continental nuclei. Science, 164: 1229~1242.
[33]
Jahn B M, Wu F, Hong D. 2000a. Important crustal growth in the Phanerozoic: Isotopic evidence of granitoids from east-central Asia. Proc. Indian Acad. Sci. (Earth Planet Sci. ), 109 (1): 5~20.
[34]
Kovalenko V I, Yarmolyuk V V, Vladikin N V, Ivanov V G, Kovach V P, Kozlovsky A M, Kostitisin Yu A, Kotov A B, Salnikova E B. 2002. Epoch of formation, geodynamic setting and sources of bearing rare metal magmatism in Central Asia. Petrology, 10(3):227~253 (in Russian).
[35]
Martin H. 1986. Effect of steeper Archean geothermal gradient on geochemistry of subduction zone magmas. Geology, 14:753 ~756.
[36]
McCulloch M T, Bennett V C. 1994. Progressive growth of the earth\' s continental crust and depleted mantle: Geochemical constraints.Geochim. et Cosmochim. , 58: 4717~4738.
[37]
Patchett P J. 1992. Isotopic studies of Proterozoic crustal growth and evolution. In: Condie K C, ed. Proterozoic Crustal Evolution.Amsterdam: Elsevier, 481~508.
[38]
Stein M, Hofmann A W. 1994, Mantle plumes and episodic crustal growth. Nature, 372: 63~ 68.
[39]
van der Voo R, Sparkman W, Bijwaard H. 1999. Mesozoic subducted slabs under Siberia. Nature, 397: 246~249.
[40]
Veevers J J. 1994. Pangea: evolution of a supercontinent and its consequences for earth\' s paleoclimate and sedimentary environments. In: Klein G D, ed. Pangea, Paleoclimate,Tectonics, and Sedimentation during Accretion, Zenith, and Breakup of a Supercontinent. Boulder,Colorado, Geol. Soc. Am.Spec. Paper 288: 13~23.
[41]
Yarmolyuk V V, Kovalenko V I, Kuzmin M I. 2000. North Asia superplume in the Phanerozoic: magmatism and geodynamics.Geotectonics, (5): 3~29 (in Russia with English abstract).