Blichert-Toft J, Albarède F. 1997. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth Planet Sci Lett, 148: 243-258
[4]
Bonin B. 2007. A-type granites and related rocks: Evolution of a concept, problems and prospects. Lithos, 97: 1-29
[5]
Chung S L, Liu D, Ji J, et al. 2003. Adakites from continental collision zones: Melting of thickened lower crust beneath southern Tibet. Geology, 31: 1021-1024
[6]
Collins W J, Beams S D, White A J R, et al. 1982. Nature and origin A-type granites with particular reference to Southeastern Australia. Contrib Mineral Petrol, 80: 189-200
[7]
Eby G N. 1992. Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications. Geology, 20: 641-644
[8]
Frost C D, Frost B R. 2011. On ferroan (A-type) granitoids: Their compositional variability and modes of origin. J Petrol, 52: 39-53
[9]
Griffin W L, Pearson N J, Belousova E, et al. 2000. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochim Cosmochim Acta, 64: 133-147
[10]
Hou Z Q, Gao Y F, Qu X M, et al. 2004. Origin of adakitic intrusives generated during mid-Miocene east-west extension in southern Tibet. Earth Planet Sci Lett, 220: 139-155
[11]
Hu Z C, Gao S, Liu Y S, et al. 2008. Signal enhancement in laser ablation ICP-MS by addition of nitrogen in the central channel gas. J Anal At Spectrom, 23: 1093-1101
[12]
Hu Z C, Liu Y S, Gao S, et al. 2012. Improved in situ Hf isotope ratio analysis of zircon using newly designed X skimmer cone and Jet sample cone in combination with the addition of nitrogen by laser ablation multiple collector ICP-MS. J Anal At Spectrom, 27: 1391-1399
[13]
King P L, White A J R, Chappell B W, et al. 1997. Characterization and origin of aluminous A-type granites from the Lachalan Fold Belt, Southerstern Australia. J Petrol, 38: 371-391
[14]
Le Maitre R W, Bateman P, Dudek A, et al. 1989. A Classification of Igenous Rocks and Glossary of Terms. Oxford: Blackwell. 1-253
[15]
Liu Y S, Hu Z C, Gao S, et al. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chem Geol, 257: 34-43
[16]
Liu Y S, Hu Z C, Zong K Q, et al. 2010a. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Chin Sci Bull, 55: 1535-1546
[17]
Liu Y S, Gao S, Hu Z C, et al. 2010b. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths. J Petrol, 51: 537-571
[18]
Losielle M C, Wones D R. 1979. Characterisitics and origin of anorogenic granites. Geol Soc Am Abstr Prog, 11: 468
[19]
Zhu D C, Mo X X, Niu Y L, et al. 2009. Geochemical investigation of Early Cretaceous igneous rocks along an east-west traverse throughout the central Lhasa Terrane, Tibet. Chem Geol, 268: 298-312Zhu D C, Zhao Z D, Niu Y L, et al. 2011. The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth. Earth Planet Sci Lett, 301: 241-255
Maniar P D, Piccoli P M. 1989. Tectonic discrimination of granitoids. Geol Soc Am Bull, 101: 635-643
[32]
Miller C F. 1985. Are Strongly peraluminous magmas derived from pelitic sedimentary sources? J Geol, 93: 673-689
[33]
Miller C F, Mcdowell S M, Mapes R W. 2003. Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance. Geology, 31: 529-532
[34]
Qu X M, Hou Z Q, Zhou S G. 2002. Geochemical and Nd, Sr isotopic study of the post-orogenic granites in the Yidun arc belt of northern Sanjiang region, southwestern China. Resour Geol, 52: 163-172
[35]
Reid A J, Fowler A P, Phillips D, et al. 2005a. Thermochronology of the Yidun Arc, central eastern Tibetan Plateau: Constraints from 40Ar/39Ar K-feldspar and apatite fission track data. J Asian Earth Sci, 25: 915-935
[36]
Reid A J, Wilson C J L, Phillips D, et al. 2005b. Mesozoic cooling across the Yidun Arc, central-eastern Tibetan Plateau: A reconnaissance Ar40/Ar39 study. Tectonophysics, 398: 45-66
[37]
Reid A J, Wilson C J L, Liu S. 2005c. Structural evidence for the Permo-Triassic tectonic evolution of the Yidun Arc, eastern Tibetan plateau. J Struct Geol, 27: 119-137
[38]
Reid A J, Wilson C J L, Shun L, et al. 2007. Mesozoic plutons of the Yidun Arc, SW China: U/Pb geochronology and Hf isotopic signature. Ore Geol Rev, 31: 88-106
[39]
Sun S S, Mcdonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. Geol Soc London Spec Publ, 42: 313-345
[40]
Watson E B, Harrison T M. 1983. Zircon saturation revisited: Temperature and composition effects in a variety of crustal magma types. Earth Planet Sci Lett, 64: 295-304
[41]
Weislogel A L. 2008. Tectonostratigraphic and geochronologic constraints on evolution of the northeast Paleotethys from the Songpan-Ganzi Complex, central China. Tectonophysics, 451: 331-345
[42]
Whalen J B, Currie K L, Chappell B W. 1987. A-type Granites: Geochemical characteristics, discrimination and petrogenesis. Contrib Mineral Petrol, 95: 407-419
[43]
Xu J F, Shinjo R, Defant M J, et al. 2002. Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust? Geology, 30: 1111-1114
[44]
Zhao X F, Zhou M F, Li J W, et al. 2008. Association of Neoproterozoic A- and I-type granites in South China: Implications for generation of A-type granites in a subduction-related environment. Chem Geol, 257: 1-15