Burchfiel B C,Zhiliang C,Hodges K V,et al.1992.The south Tibetan detachment system,Himalayan orogen:extension contemporaneous with and parallel to shortening in a collisional mountain belt.Bouder Colorado.Geological Society of America Special Paper 269,41p.
[11]
Deng Jinfu,Zhao Hailing,Lai Shaocong,et al.1994.Generation of muscovite/two-mica granite and intracontinental subduction.Earth Science-Journal of China University of Geoscience,19(2):139～147(in Chinese and English abstract).
[12]
Li Tong,Rao Jilong.1963.Average chemical composition of igneous rocks in China.Acta Geologica Sinica,43(3):271～280.
[13]
Liao Zhongli,Mo Xuanxue,Pan Guitang,et al.2003.The distribution and tectonic signify cance of per-aluminous granites in southern Xizang.Sedimentary Geology and Tethyan Geology,23(3):12～20 (in Chinese with English abstract).
[14]
Murphy M A,Harrison T M,Durr S B,et al.1997.Significant crustal shortening in south-central Tibet prior to the Indo-Asian collision.Geology,25:719～722.
[15]
Nie Fengjun,Hu Peng,Jiang Sihong,et al.2005.Type and temporal-spatial distribution of gold and antimony deposits (prospects) in southern Tibet,Tibet Autonomous Region,China.Acta Geologica Sinica,79(3):373～385(in Chinese with English abstract).
[16]
Searle M P,Parrish R R,Hodges K V,et al.1997.Shisha Pangma eucogranite,south Tibetan Himalaya:field relations,geochemistry,age,origin,and emplacement.J.Geol.,105:195～317.
[17]
Yin A,Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan orogen.J.Ann.Rev.Earth Planet.Sci.,28:211～280.
[18]
Yuan Xuecheng,Li Li,Fan Wenke,et al.1990.Magne-telluric current sounding on crust and upper mantle of Lhozag-Nakqu district,Tibet.In:Chinese Academy of Geology,ed.Himalayan lithospheric tectonic evolution--Xizang GeophysicalContributions.Beijing:Geological Publishing House,63～71 (in Chinese).
Wang Zhonggang,Yu Xueyuan,Zhao Zhenhua.1989.Rare earth element geochemistry.Beijing:Science Press,1～535 (in Chinese)
[22]
Xizang Bureau of Geology and Mineral Resources (XZBGMR).1993.Regional geology of Xizang Autonomous Region.Beijing:Geological Publishing House,1～707 (in Chinese with English abstract).
Chengdu Institute of Geology and Mineral Resources,China Geological Survey.2004.Geological map and its explanation note of Qinghai-Tibet plateau.Chengdu:Chengdu Map Publishing House,1～133(in Chinese).
[30]
Department of Geology,Nanjing University.1984.Geochemisty.Beijing:Science Press,259～252(in Chinese).
[31]
Guiyang Institute of Geochemistry,Chinese Academy of Science.1977.Concise handbook of geochemistry.Beijing:Science Press,P:69～72(in Chinese).
[32]
Li Dewei,Liu Demin,Liao Qun\'an,et al.2003.Definition and significance of the Lhagoi Kangri metamorphic core complexs in Sa\'gya,southern Tibet.Geological Bulletin of China,22(5):303～307(in Chinese with English abstract).
[33]
Murphy M A,Harrison T M.1999.Relationship between leucogranites and the Qomolangma detahmet in the Rongbuk Valley,South Tibet.Geology,27:831～834.
[34]
Romer R L,Forster H J,Breitkreuz C.2001.Intracontinental extensional magmatism with a subduction fingerprint:the late Carboniferous Halle volcanic complex (Germany).Contributions to Mineralogy and Petrology,41:201～221.
[35]
Tong Jinsong,Zhong Huaming,Xia Jun,et al.2003.Geochemical features and tectonic selting of peraluminous granite in the Lhozag area,Southern Tibet.Geological Bulletin of China,22(5):308～318 (in Chinese with English abstract).
[36]
Tu Kuangchih,Zhang Yuquan,Zhao Zhenhua,et al.1981.Characteristics and evolution of granitoids of South Xizang(Tibet).Geochimica,(1):1～7(in Chinese with English abstract).
[37]
Wang Shi,Lu Deyuan,Huang Liyan,et al.1990.Structural model and velocity distributing features of N-striking crust in Tibet plateau.In:Chinese Academy of Geology,eds.Himalayan lithospheric tectonic evolutionXizang Geophysical Contributions.Beijing:Geological Publishing House,38～50 (in Chinese).
[38]
Zhang Yuquan,Wang Zhonggang,Zhao Zenhua,et al.1981.On the crustal movement characteristic of the Xizang plateau with special reference to intermediate-acid magmatic activities.Geochimica,(2):136～141(in Chinese with English abstract).
