Blichert-Toft J and Albarède F. 1997. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth and Planetary Science Letters, 148(1?2): 243?258.
[14]
Blisniuk P M, Hacker B R, Glodny J, Ratschbacher L, Bi S W, Wu Z H, Mcwilliams M O and Calvert A. 2001. Normal faulting in central Tibet since at least 13.5 Myr ago. Nature, 412(6847): 628?632.
[15]
Collins W J, Beams S D, White A J R and Chappell B W. 1982. Nature and origin of A-type granites with particular reference to southeastern Australia. Contributions to Mineralogy and Petrology, 80(2): 189?200.
[16]
DeCelles P G, Gehrels G E, Najman Y, Martin A J, Carter A and Garzanti E. 2004. Detrital geochronology and geochemistry of Cretaceous-Early Miocene strata of Nepal: Implications for timing and diachroneity of initial Himalayan orogenesis. Earth and Planetary Science Letters, 227(3?4): 313?330.
[17]
Eby G N. 1992. Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications. Geology, 20(7): 641?644.
[18]
Griffin W L, Pearson N J, Belousova E, Jackson S E, van Achterbergh E, O’Reilly S Y and Shee S R. 2000. The Hf isotope composition of cratonic mantle: LA-MC- ICPMS analysis of zircon megacrysts in kimberlites. Geochimica et Cosmochimica Acta, 64(1): 133?147.
[19]
Rowley D B. 1996. Age of initiation of collision between India and Asia: A review of stratigraphic data. Earth and Planetary Science Letters, 145(1?4): 1?13.
[20]
Rubatto D. 2002. Zircon trace element geochemistry: Partitioning with garnet and the link between U-Pb ages and metamorphism. Chemical Geology, 184(1?2): 123?138.
[21]
S?derlund U, Patchett P J, Vervoort J D and Isachsen C E. 2004. The 176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions. Earth and Planetary Science Letters, 219(3?4): 311?324.
[22]
Vervoort J D and Jonathan P P. 1996. Behavior of hafnium and neodymium isotopes in the crust: Constraints from Precambrian crustally derived granites. Geochimica et Cosmochimica Acta, 60(19): 3717?3733.
[23]
Whalen J B, Currie K L and Chappell B W. 1987. A-type granites: Geochemical characteristics, discrimination and petrogenesis. Contributions to Mineralogy and Petrology, 95(4): 407?419.
[24]
Williams H, Turner S, Kelley S and Harris N. 2001. Age and composition of dikes in Southern Tibet: New constraints on the timing of, east-west extension and its relationship to postcollisional volcanism. Geology, 29(4): 339?342.
[25]
Wright J B. 1969. A simple alkalinity ratio and its application to questions of non-orogenic granite genesis. Geological Magazine, 106(4): 370?384.
Amelin Y, Lee D C and Halliday A N. 2000. Early-middle archaean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains. Geochimica et Cosmochimica Acta, 64(24): 4205?4225.
[32]
Barbarin B. 1999. A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos, 46: 605?626.
[33]
Batchelor R A and Bowden P. 1985. Petrogenetic interpretation of granitoid rock series using multicationic parameters. Chemical Geology, 48(1?4): 43?55.
[34]
Liu Y, Hu Z, Zong K, Gao C, Gao S, Xu J and Chen H. 2010. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Chinese Science Bulletin, 55(15): 1535?1546.
[35]
Ludwig K R. 2003. User’s Manual for Isoplot/Ex Version 2.05. Berkeley, US: Berkeley Geochronology Center: 1?272.
[36]
Maniar P D and Piccoli P M. 1989. Tectonic discrimination of granitoids. Geological Society of America Bulletin, 101(5): 635?643.
[37]
McDonough W F and Sun S S. 1995. The composition of the earth. Chemical Geology, 120(3?4): 223?253.
[38]
Morel M L A, Nebel O, Nebel J Y J, Miller J S and Vroon P Z. 2008. Hafnium isotope characterization of the GJ-1 zircon reference material by solution and laser-ablation MC-ICP-MS. Chemical Geology, 255(1?2): 231?235.
[39]
Pearce J A. 1996. Sources and settings of granitic rocks. Episodes, 19(4): 120?125.