Bllsnluk P M, Hacker B, Glodny J, Ratschbacher L, Bill S, Wu Z H, McWilliams M O, Calvert A. 2001. Normal faulting in central Tibet since at least 13.5 Myr ago. Nature, 412: 628-632.
[2]
Chen Bingwei, Ren Liudong, Wang Yanbin. 2000. the geotectonic and deformation characteristic for the Oinghai--Xizang plateau and adjacent areas. In: Xiao Xuchang, Li Tingdong ads. Tectonic evolution and uplifting mechanism of the Oinghai-- Xizang plateau. Guangzhou: Guangdong science and technology press, 85-122.
[3]
Ding L, Zhong D L, Yin A, Harrison T M. 2001. Cenozoic structural and metamorphic evolution of the eastern Himalayan syntaxis (Namehe Barwa). Earth Planet. Sci. Lett., 192: 423-438.
[4]
Hou Zengqian, Li Zhenqing, Qu Xiaoming et al. 2001. The uplifting processes of the tibetan plateau since 0. 5Ma B. P.:evidences from hydrothermal activity in the Gangdise belt. Science in China (Series D), 44 (sup.) : 35-44.
[5]
Hou Zengqian, Mo Xuanxue, Gao Yongfeng et al. 2003c. Adakite, a possible host rock porphyry copper deposits: case studies of porphyry copper belts in Tibetan plateau and in northern Chile. Mineral deposits, 22(1) : 1-12.
[6]
Kind R, Ni J, Zhao W, et al. 1996. Evidence from earthquake data for a partially molten crustal layer in southern Tibet. Science, 274.. 1692-1694.
[7]
Makovsky Y, Klemperer S L. 1999. Measuring the seismic properties of Tibetan bright spots: evidence for free aqueous fluids in the Tibetan middle crust. J. Geophys. Res., 104: 10795-10825.
[8]
Ni J, York J. 1978. Late Cenozoic tectonics of the Tibetan plateau. J Geophys Res, 83:5377-5384.
[9]
Shen Xianjie, Zhang Wenren, Yang Shuzhen, et al. 1990. Heat flow and heat evolvement of terrain tectonic in Qinghai--Xizang plateau. , 1-90.
[10]
Tong Wei, Zhang Mingtao, Zhang Zhifei, et al. 1981. Geothermal in the Xizang plateau. Beijing: Science Press.
[11]
Wei Wenbo, Martyn Unsworth, Alan Jones, et al. 2001. Detection of widespread fluids in the Tibetan crust by magnetotelluric studies.Science, 292: 716-718.
[12]
Williams H, Turner S, Kelley S, Harris N. 2001. Age and composition of dikes in Southern Tibet: new constraints on the timing of east-west extension and It\\'s relationship to post- collisional volcanism. Geology, 29:339-342.
[13]
Yokoyama T, Nakai S, Waikita H. 1999. Helium and carbon isotopic compositions of hot spring gases in the Tibetan plateau. J. Volcan. Geotherm. Res. , 88: 99-107.
[14]
Zhang Zhifei, Zhu Meixiang, Liu Shibin. 1982. Primary research about hydrothermal geochemistry in Tibet. Transaction of the Peking University,(3):88-96.
[15]
Zhao Ping, Jin Jian, Zhang Haizheng, et al.1998. Chemical composition of thermal water in the Yangbajing geothermal field, Tibet. Chinese Science Bulletin, 33(1) : 61-72.
[16]
Zhu Bingqiu, Zhu Lixin, Shi Changyi, et al. 1992. Geochemical exploration in geothermal field. Beijing: Geological Press.
Andrews J N. 1985. The isotopic composition of radiogenic helium and its use to study groundwater movement in confined aquifers. Chem. Geology, 49: 339-350.
Brown L D, Zhao W J, Nelson K D, et al. 1996. Bright spots, structure, and magmatism in southern Tibet from INDEPTH serimie reflection profiling. Science, 274.. 1688-1690.
[39]
Coleman M, Hodges K. 1995. Evidence for Tibetan plateau uplift before 14 Myr ago from a new minimum age for east-west extension. Nature, 374: 49-52.
[40]
Hoke L, Lamb S, Hilton D, Poreda R J. 2000. Southern limit of mantle-derived geothermal helium emissions in Tibet : implications for lithoshperic structure. Earth Planet. Sci. Lett. , 180: 297- 308.
[41]
Hou Zengqian, Li Zhenqing. 2004. Possible location for underthrusting front of the Indus continent: constrains fromhelium isotope of the geothermal gas in southern Tibet and eastern Tibet. Acta geologica sinica, 78(4):482-493.
[42]
Kimmelmann E S. 1996. Use of Helium isotopes in groundwater studies of the Parana Basin, Brasil. In:30th international geological congress abstracts. 3(3): 238.
[43]
Li Zhenqing. 2002. The modern hydrothermal fluid activity during the collisional orogenesis in the Tibetan plateau. Ph.D. thesis.
[44]
Molnar P, Tapponnier P. 1978. Active tectonics of Tibet. J Geophys Res, 83:5361-5375.
[45]
Nelson K D, Zhao W J, Brown L D, et al. 1996. Parially molten middle crust beneath Southern Tibet:synthesis of project INDEPTH results. Science, 274:1684 - 1688.
[46]
Pan Yusheng, Kong Xiangru, Zhong Dalai, et al. 1998. Structure, evolution and kinetics of the lithosphere in the Qinghai--Xizang plateau. In: Sun Honglie and Zheng Du ads. Formation, evolution and development of the Qinghai--Xiang plateau. Guangzhou: Guangdong science and technology press, 1-65.
[47]
Tapponnier P, Molnar P. 1977. Active faulting and tectonics of China. J. Geophys. Res. , 82: 2905-2930.
[48]
Xia Baoben, Zhang Jiacheng. 1993. Primary research about the convention of geothermal activity in Tibet. In : collected papers of international proseminar on development and utilization of megatemperaure geothermal in Tibet, China. Beijing: Geological publishing house, 1- 7.
[49]
Yin A, Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen. J. Ann. Rev. Earth Planet. Sci., 28, 211-280.
[50]
Zhang Ligang. 1985. Application of stable isotope in geological science. Xi\\'anz Shanxl science and technology press.
[51]
Zhao W J, Nelson K D, Poject INDEPTH team. 1996. Deep seismic reflection evidence for continental underthrusting beneath the south Tibet. Nature, 366: 557-559.
[52]
Zhao Wenjin, Nelson, Che Jingkai, et al. 1996. Deep seismic reflection in Hamalaya region reveals the complexity of the crust and upper mantle. Acta Geoscientia Sinica, 17(2) : 138-152.
