Xiao Qinghui, Deng Jinfu, Ma Daquan, et al. 2002. The ways of investigation on granitoids. Beijing: Geological Publishing House,30～40 (in Chinese).
[2]
Xiao Xuchang, Wang Jun. 1998. A brief review of tectonic evolution and uplift of the Qinghai-Tibet Plateau, Geological Review, 44(4) :372～381 (in Chinese with English abstract).
[3]
Zhao Wenjin, Project INDEPTH Group. 2001. A Geophysics Study on Geological Deep-Structure of the Sutures of the Himalaya Mountain and the Yarlung Zangbo River. Beijing: Geological Publishing House, 327 ～ 349 (in Chinese).
Bureau of Geology and Mineral Resources of Xizang Autonomous Region. 1993. Regional geology of Xizang (Tibet) autonomous region. Beijing: Geological Publishing House, 388 ～ 390 (in Chinese).
[11]
Chen Peirong, Zhou Xinmin, Zhang Wenlan, et al. 2004. The origin and significance of Early Yanshan syenite-granitoids in the Nanling region. Science in China, 34 (6): 493 ～ 503 (in Chinese).
[12]
Gao Rui, Li Tingdong, Wu Gongjian. 1998. Lithospheric evolution and geodynamic process of the Qinghai-Tibet Plateau:Aninspiration from the Yadong-Golmud-Ejin geoscience transect.Geological Review, 44(4):389～395 (in Chinese with English abstract).
[13]
Garzione C N, Dettman D L, Quade J, et al. 2000. Hight times on the Tibetan Plateau: Paleoelevation of the Thakkola graben,Nepal. Geolgy, 28: 339～342.
[14]
Harrison T M, Armstrong R L, Naeser C W. 1979. Geochronology and thermal history of the coast plutonic complex near Prince Rupert, British Columbia. Can. J. Earth Sci. , 16:400～410.
[15]
Harrison T M, Copeland P, Kidd W S F, et al. 1995. Activation of the Nyainqentanghla shear zone: implications for uplift of the southern Tibetan Plateau. Tectonics, 14(3): 658～676.
[16]
Harrison T M, Grove M, Lovera O M, et al. 1998. A model for the origin of Himalaya anatexis and inverted metamorphism. J.Geophys. Res. , 103:27017～27032.
[17]
Lee J K W, Williams I S, Ellis D J. 1997. Pb, U and Th diffusion in natural zircon. Nature, 390: 159～162.
[18]
Liegeois J P, Navez J, Hertogen J, et al. 1998. Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and peralkaline granitoids. The use of sliding normalization.Lithos. , 45:1～28.
[19]
Lü Qingtian, Jiang Mei, Ma Kaiyi, et al. 1996. Travel time tomography inversion and the deep structure of the southern Tibet. Acta Seismologica Sinica, 18 (4): 451 ～ 459 (in Chinese ).
[20]
Peter M B, Bradley R H, et al. 2001. Normal faulting in central Tibet since at least 13.5 Myr ago. Nature, 412: 628～632.
[21]
Sylvester P J. 1998. Post-collision strongly peraluminous granites.Lithos. , 45: 29 ～ 44.
[22]
Wagner G, Van Den Haute P. 1992. Fission track dating. Dordrecht:Kluwer Academic Publishers, 1 ～275.
[23]
Williams H, Turner S, Kelley S, et al. 2001. Age and composition of dikes in Southern Tibet: New constraints on the timing of eastwest extension and its relationship to postcollisional volcanism.Geologe, 29: 339～342.
[24]
Wu Gongjian, Xiao Xuchang, Li Tingdong. 1989. Yardong-Golmud geoscience transect in Qinghai-Xizang (Tibet) Plateau. Acta Geologica Sinica, 63 (4): 285 ～ 296 (in Chinese with English abstract).
Achache J, Courrillot V, Zhou Yaoxin. 1984. Paleogeographic and tectonic evolution of southern Tibet since Middle Cretaceous time:new paleomagnetic data and synthesis. J. Geophys. Res. , 89:10311～10399.
[31]
Besse J, Courtillou V, Possi J P, Westphal M, et al. 1984.Paleomagnetic estimates of crustal shortening in the Himalayan thrusts and Zangbo suture. Nature, 311: 621～626.
[32]
Edwards M A, Harrison T M. 1997. When did the roof collapse? Late Miocene north-south extension in the High Himalaya revealed by the Th-Pb monazite dating of the Khula Kangri granite. Geology,25:543～546.
[33]
Harris N, Massey J. 1994. Decompression and anatexis of Himalayan metapelites. Tectonics, 13:1537～ 1546.
[34]
Jaeger J J, Courtillot V, Tapponnier P. 1989. Paleontological view of the ages of the Deccan traps, the Cretaceous/Tertiary boundary and the India-Asia collision. Geology,17: 316～319.
[35]
Jin Chengwei, Harris N B W, Xu Ronghua, et al. 1990. Plutonic rocks of the 1985 Tibet Geotraverse, Lhasa to Golmud. The geology evolution of the Tibetan Pleteau. Beijing: Science Press,141～172 (in Chinese with English abstract).
[36]
Kidd W S F, Pan Y, Chang C, et al. 1988. Geological mapping of the 1985 Chinese-British Tibetan ( Xizang-Qinghai ) Plateau geotraverse route. Phil. Trans. Roy. Soc, London A, 327:287～305.
[37]
Liegeois J P. 1998. Some words on the post-collisional magmatism.Lithos. , 45: 15～17.
[38]
Liu Qisheng, Wu Zhenhan, Hu Daogong, et al. 2003. SHRIMP UPb zircon dating of the Nyainqentanglha Granite. Chinese Science Bulletin,48 (20): 2170～2175 (in Chinese).
[39]
Nam T N, Sano Y, Terada K, et al. 2001. First SHRIMP U-Pb zircon dating of granulites from the Kontum massif (Vietnam)and tectonothermal implications. Journal of Asian Earth Sciences,19:77～84.
[40]
Searle M P, Parrish R R, Hodges K V A, et al. 1997. Shisha Pangma leucogranite, south Tibetan Himalaya: field relations,geochemistry, age, origin and emplacement. Journal of Geology,105:295～317.
[41]
Tugner D L, Forbes R B. 1976. K-Ar studies in two deep basement drill holes: a new geological estimate of blocking for biobite.Eos. ,57: 353.
[42]
Willems H, Zhou Z, Zhang B, et al. 1996. Stratigraphy of the Upper Cretaceous and Lower Tertiary strata in the Tethyan Himalayas of Tibet (Tingri area, China). Geol. Rundsch, 85: 723～754.
[43]
Wu C, Nelson K D, Wortman G, et al. 1998. Yadong cross structure and south Tibetan detachment in the east central Himalaya.Tectonics, 17(1) :28～45.
[44]
Xiao Xuchang, Li Tingdong. 2000. Tectonic Evolution and Uplift of Qinghai-Xizang (Tibet) Plateau. Guangzhou: Guangdong Science and Technology Press, 1～313 (in chinese).
[45]
Xu R H, Scharer U, Allegre C J. 1985. Magmatism and metamorphism in the Lhasa block (Tibet): a geochronological study. Journal of Geology, 93 : 41 ～ 57.
[46]
Yin A, Harrison T M. 2000. Geologic evolution of the HimalayanTibetan orogen. Annu. Rev. Earth Planet. Sci. Lett., 28: 211～280.
