[9]Harrison T M, Yin A, Grove M, et al. 2000. Displacment history of the Gangdese thrust, Southeastern Tibet[J]. J. Geophys. Res., 105: 19211~19230.
[2]
[10]Hou Z Q, Qu X M, Huang W, et al. 2001.The Gangdese porphyry copper belt: the second significant porphyry belt in Tibetan plateau [J]. China Geology, 28(1): 27~29(in Chinese with English abstract).
[3]
[11]Hou Z Q, Qu X M, Wang S X, et al. 2003a. Re-Os age for molybdenites from the Gaogdese porphyry belt in the Tibetan plateau: implication to mineralization duration and geodynamic setting[J].Science in China(Series D), (in press).
[4]
[12]Hou Z Q, Mo X X, Gao Y F, et al. 2003b. Adakite, a possible host rock for porphyry copper deposits: case studies of porphyry copper belts in Tibetan platean and in northern Chile[J]. Mineral Deposits, 22(1): 1~12(in Chinese with English Abstract).
[5]
[13]Hou Z Q , Mo X X , Qu X M, et al. 2003. The mid-Miocene potassic adakite generation related to interaction of subducted Neo-Tethyan slab with overlying Asian mantle in South Tibet[J]: Earth Planet. Sci. Lett., (in press).
[6]
[14]Kay R W and Kay S M. 1994. Delamination and delamination Magmatism[J]. Tectonophysics, 219:177~189.
[7]
[15]Leeder M R, Smith A B and Yin J.1988. Sedimmentology, palaeoecology and palaoenvironmental evolution of the 1985 Lhasa to Golmud Geotraverse[J]. Phil. Trans. Roy. Soc. Lond., A327:107~143.
[8]
[16]Ludwig K. 1999. A geochrological toolkit for Microsoft Excel[M]. Geochronology Center, Berkeley, Special Publication 1a. Isoplot/Ex, version 2.0.
[9]
[17]Molnar P and Tapponnier P. 1978. Active tectonics of Tibet[J]. J. Geophys. Res., 83: 5361~5375.
[10]
[18]Pierce J A and Mei H.1988. Volcanic rocks of the 1985 Tibet Geotraverse Lhasa to Golmud[J]. Phil. Trans. Roy. Soc. Lond., A327:203~213.
[11]
[19]Qu X M, Hou Z Q and Huang W. 2001. Gangdese porphyry copper belt: the second Yulong porphyry copper belt in Tibet [J]? Mineral Deposits, 20(4): 355~366(in Chinese with English abstract).
[12]
[20]Qu X M, Hou Z Q and Li Z Q. 2003. 40Ar/39Ar ages of the ore-bearing porphyry of the Gangdese porphyry copper belt and their geological significances[J]. Acta Geologica Sina,(in press).
[13]
更多...
[14]
[21]Schǎer U, Xu R H and All閞e C J. 1984. U-Pb geochronology of the Gangdese (Transhimalaya) plutonism in the Lhasa-Xizang region, Tibet[J]. Earth Planet. Sci. Lett., 69: 311~320.
[15]
[22]Shirey S B and Walker R J. 1995. Carius tube digestion for low-blank rhenium- osmium analysis[J]. Anal. Chem., 67:2136~2141.
[1]Bllsnluk P M, Hacker B, Glodny J, et al. 2001. Normal faulting in central Tibet since at least 13.5 Myr ago[J]. Nature, 412:628~632.
[20]
[2]Cheng L J, Li Z, Liu H F, et al. 2001. Basic features of the east Gangdese polymetallic metallogenic belt[J].Tibet Geology, 19(1):43~53(in Chinese with English abstract).
[21]
[3]Coleman M and Hodges K. 1995. Evidence for Tibetan Plateau uplift before 14 Ma ago from a new minimum age for east-west extension[J]. Nature, 374:49~52.
[22]
[4]Dewey J F, Shackelton R M, Chang C, et al. 1988. The tectonic evolution of the Tibetan plateau[J]. Phil. Trans. Roy. Soc. Lond., A327:379~413.
[23]
[5]Du A D, He H L and Yin W N. 1994. The study on the analytical methods of Re-Os age for molybdenites[J]. Acta Geologica Sinica, 68(4): 339~346 (in Chinese with English abstract).
[24]
[6]Du G S, Yao P, Pan F C, et al. 1998. Exhalogenic skarn and mineralization, exampled by Jiama copper polymetallic deposit of Xizang[M]. Chengdu: Sichuang Sci. & Tech. Press (in Chinese with English abstract).
[25]
[7]Feng X L, Guan S P, Mou C L, et al. 2001. Geologcal characteristics and gensis of the Jiama copper polymetallic deposit in Tibet[J]. Geology-Geochemistry, 29(4): 40~48(in Chinese with English abstract).
[26]
[8]Harris N B W, Xu R, Lewis C L, et al. 1988. Isotope geochemistry of the 1985 Tibet Geotraverse, Lhasa to Golmud[J]. Phil. Trans. Roy. Soc. Lond., A327:263~285.
[27]
[23]Simoliar M I, Walker R J and Morgan J W. 1996. Re-Os ages of group IIA, IIIA, IVA and VIB iron meteorites[J]. Science, 271: 1099~1102.
[28]
[24]Stein H J, Markey R J, Morgan J W, et al. 1997. Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenite belt, Shananxi province, China[J]. Econ. Geol., 92: 827~835.
[29]
[25]Turner S, Hawkesworth C, Liu J Q, et al. 1993. Timing of Tibetan uplift constrained by analysis of volcanic rocks[J]. Nature, 364: 50~54.
[30]
[26]Wang Q H, Wang B S, Li J G, et al. 2002. Basic features and ore prospect evaluation of the Gangdeseisland arc, Tibet, and its copper polymetallic ore belt[J]. Geological Bulletin of China, 21(1): 35~40(in Chinese with English abstract).
[31]
[27]Xu R H, Schǎer U and All閞e C J. 1985. Magmatism and metamorphism in the Lhasa block(Tibet): a geochronological study[J]. J. Geol., 93: 41~57.
[32]
[28]Yin J, Xu J, Liu C, et al. 1988. The Tibetan plateau: regional stratigraphic context and previous work[J]. Phil. Trans. Roy. Soc. Lond., A327:5~52.
[33]
[29]Yin A and Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen: Annu. Rev[J]. Earth Planet. Sci., 28: 211~280.
[34]
[30]Zheng Y Y, Wang B S, Fan Z H, et al. 2002. Analysis of tectonic evolution in the eastern section of the Gangdese Mountains, Tibet and the metallogenic potentialities of copper gold polymetal[J]. Geological Science and Technology Information, 21(2):55~60(in Chinese with English abstract).