Dunlap W J, Weinberg R F and Searle M P. 1998.Karakoram fault zone rocks cool in two phase. J Geol Soc London, 155: 903-912.
[6]
Hou Z Q, Ma H W, Khin Zaw, Zhang Y Q, Wang M J, Wang Z and Pan G T. 2003.The Himalayan Yulong porphyry Copper belt: Product of Large?scale strike?slip faulting in Eastern Tibet. Economic Geology, 98: 125-145.
[7]
Hou Z Q, Zeng P S and Gao Y F. 2006.The Himalayan Cu?Mo?Au mineralization in the eastern Indo?asian collision zone: Constraints from Re?Os dating of molybdenite. Minerlium Deposita, 41: 33-45.
[8]
Richards T P. 2001.Discussion of "Is there a close spatial relationship between faults and plutons" ? Journal of Structural Geology, 23: 2025-2027.
[9]
Richards T P. 2003.Tectono?magmatic precursors for porphyry Cu?(Mo?Au) deposit formation. Economic Geology, 98: 1515-1533.
[10]
Roger F, Tapponnier P, Arnaud N, Scharer U, Brunel M, Xu Z and Yang J. 2000.An Eocene magmatic belt across central Tibet: Mantle subduction triggered by the Indian collision? Terra Nova, 12: 102-108.
Armijo R, Tapponnier P and Han T. 1989.Late Cenozoic right?lateral strike?slip faulting across southern Tibet. J Geophys Res, 94: 2787-2838.
[26]
Brown M. 1994.The generation, segregation, ascent and emplacement of granite magma: The migmatite?to?crustally?derived granite connection in thickened orogens. Earth?Science Reviews, 36: 83-130.
[27]
Coleman M E and Hodges K P. 1993.Evidence for Tibetan plateau uplift before 14 Myr ago from a new minimum estimate of east?west extension. Nature, 364: 50-54.
[28]
Cooke D R, Hollings P and Walshe J L. 2005.Giant porphyry deposits: Characteristics, distribution, and tectonic controls. Economic Geology, 100(5): 801-818.
[29]
Cornejo P, Tosdal R M, Mpodozis C, Tomlinson A J, Rivera O and Fanning C M. 1997.El Salvador, Chile porohyry copper deposit revisited: Geological and geochronoligic framework. International Geology Review, 39: 22-54.
[30]
Kapp P, Murphy M A, Yin A and Harrison T M. 2003.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet. Tectonics, 22 (4): 1-23.
[31]
Lee H Y, Chung S L, Wang J R, Wen D J, Lo C H, Tsanyao F, Yang T F, Zhang Y Q, Xie Y W, Lee T Y, Wu G Y and Ji J Q. 2003.Miocene Jiali faulting and its implications for Tibet tectonic evolution. Earth and Planetary Science Letters, 205: 185-194.
[32]
Leloup P H, Lacassin R, Tapponnier P, Scharer U, Zhong Dalai, Liu Xiaohan, Zhang Liangshang, Ji Shaocheng and Trinh P T. 1995.The Ailao Shan?Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina. Tectonophysics, 251: 3-84.
[33]
Mo X X, Hou Z Q, Niu Y L, Dong G C, Qu X M, Zhao Z D and Yang Z M .2007.Mantle contributions to crustal thickening during continental collision: Evidence from Cenozoic igneous rocks in southern Tibet. Lithos, 96: 225-242.
[34]
Tapponnier P, Xu Z Q, Roger F, Meyer B, Arnaud N O, Wittlinger G and Yang J S. 2001.Oblique stepwise rise and growth of the Tibet plateau. Science, 294: 1671-1677.
[35]
Wang E and Burchfiel B C. 1997.Interpretation of Cenozoic tectonics in the right?lateral accommodation zone between the Ailao Shan shear zone and the eastern Himalayan syntaxis. Int Geol Rev, 39: 191-219.
[36]
Wang E and Burchfiel B C. 2000.Late Cenozoic to Holocene deformation in southwestern Sichuan and a adjacent Yunnan, China, and its role in formation of the southeastern part of the Tibetan Plateau. Geological Society of American Bulletin, 112(3): 413-423.
[37]
Williams H, Turner S, Kelley S and Harris N. 2001.Age and composition of dikes in Southern Tibet: News on the timing of constraints on the timing of east?west extension and its relationship to postcollisional volcanism. Geology, 29(4): 339-342.
[38]
Yin A and Harrison T M. 2000.Geologic evolution of the Himalayan?Tibetan orogen. Annu Rev Earth Planet Sci, 28: 211-280.