Zhang H F, Sun M, Zhou X H, et al. 2003. Secular evolution of the lithosphere beneath the eastern North China Craton: Evidence from Mesozoic basalts and high-Mg andesites. Geochim Cosmochim Acta, 67: 4373-4387
Anderson D L. 2000. The thermal state of the upper mantle: No role for mantle plumes. Geophys Res Lett, 27: 3623-3626
[18]
Anderson D L. 2005. Large igneous provinces, delamination, and fertile mantle. Elements, 1: 271-257
[19]
Gao S, Rudnick R L, Yuan H L, et al. 2004. Recycling lower continental crust in the North China Craton. Nature, 432: 892-897
[20]
Gao S, Rudnick R L, Xu W L, et al. 2008. Recycling deep cratonic lithosphere and generation of intraplate magmatism in the North China Craton. Earth Planet Sci Lett, 270: 41-53
[21]
Grove T L. 1981. Use of FePt alloys to eliminate the iron loss problem in 1 atmosphere gas mixing experiments: Theoretical and practical considerations. Contrib Mineral Petrol, 78: 298-304
[22]
Johnston A D, Wyllie P J. 1989. The system tonalite-peridotite-H2O at 30 kbar, with applications to hybridization in subduction zone magmatism. Contrib Mineral Petrol, 102: 257-264
[23]
Kelemen P B. 1995. Genesis of high Mg# andesites and the continental crust. Contrib Mineral Petrol, 120: 1-19
[24]
Liang Y. 2010. Multicomponent diffusion in molten silicates: Theory, experiments, and geological applications. Rev Mineral Geochem, 72: 409-446
[25]
Liu Y S, Gao S, Lee C, et al. 2005. Melt-peridotite interactions: Links between garnet pyroxenite and high-Mg# signature of continental crust. Earth Planet Sci Lett, 234: 39-57
[26]
Pearce J A, Laan S R V D, Arculus R J, et al. 1992. Boninite and harzburgite from leg 125 (Bonin-Mariana forearc): A case study of magma genesis during the initial stages of subduction. Proc Ocean Drill Prog Sci Result, 125: 623-659
[27]
Rapp R P, Shimizu N, Norman M D, et al. 1999. Reaction between slab-derived melts and peridotite in the mantle wedge experimental constraints at 3.8 GPa. Chem Geol, 160: 335-356
[28]
Sekine T, Wyllie P J. 1982. The system granite-peridotite-H2O at 30 kbar, with applications to hybridization in subduction zone magmatism. Contrib Mineral Petrol, 81: 190-202
[29]
Shimoda G, Tatsumi Y, Nohda S, et al. 1998. Setouchi high-Mg andesites revisited: Geochemical evidence for melting of subducting sediments. Earth Planet Sci Lett, 160: 479-492
[30]
Xu W L, Hergt J M, Gao S, et al. 2008. Interaction of adakitic melt-peridotite: Implications for the high-Mg# signature of Mesozoic adakitic rocks in the eastern North China Craton. Earth Planet Sci Lett, 265: 123-137
[31]
Xu Y G. 2001. Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean Craton in China: Evidence, tming and mechanism. Phys Chem Earth, 26: 747-757
