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.
[2]
Boiron M C, Dubessy J, Andre N, et al. 1991. Analysis of monoatomic ions in dividual fluid inclusions by laser-produced plasma emission spectroscopy[J]. Geochim. Cosmochim. Acta, 55: 917~923.
[3]
Bodnar R J. 1994. Synthetic fluid inclusions(XII): the system H2O-NaCl experimental determination of the halite liquidus and isochors for a 40wt%NaCleq solution[J]. Geochim. Cosmochim Acta, 58: 1053~1063.
[4]
Bodnar R J. 1995. Fluid-inclusion evidence for a magmatic source for metals in porphyry copper deposits[J]. Mineralogical Association of Canada Short Course Series, 23: 139~152.
[5]
Candela P A and Holland H D. 1986. A mass transfer modle for copper and molybdenum in magmatic hydrothermal system: the origin of porphyry-type ore deposits[J]. Econ. Geol., 81: 1~19.
[6]
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).
[7]
Chou I M. 1987. Phase relations in the system NaCl-H2O(III): solubilities of halite in vapor-saturated liquids above 445℃ and redetermination of phase equilibrium properties in the system NaCl-H2O to 1000℃ and 1500 bars[J]. Geochim. Cosmochim. Acta, 15: 1965~1975.
[8]
Cline J S and Bodnar R J. 1994. Direct evolution of brine from a crystallizing silicic melt at the Queta, New Mexico, Molybdenum deposit[J]. Econ. Geol., 89: 1780~1802.
[9]
Cloke P L and Kesler S E. 1979. The halite trend in hydrothermal solutions[J]. Econ. Geol., 74: 1823~1831.
[10]
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.
[11]
Crerar D A and Barnes H L. 1976. Ore solution chemistry(V): solubilities of chalcopyrite assemblages in hydrothermal solution at 200 to 350℃[J]. Econ. Geol., 71: 772~794.
[12]
Dammam K M S, Touret L R J, Rieffe C E, et al. 1996. PIXE and EM analyses of fluid inclusions in quartz crystals from the K-alteration zone of the Rosia Poieni porphyry-Cu deposit, Apuseni Mountains, Rumania[J]. European Journal of Mineralogy, 8: 1081~1096.
[13]
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.
[14]
Diamond I W, Marshall D D, Jackman J A, et al. 1990. Elemental analysis of individual fluid inclusions in minerals by secondary ion mass spectrometry(SIMS): application to cation ratios of fluid inclusions in an Archaean mesothermal gold-quartz vine[J]. Geochim. Cosmochim. Acta, 54: 545~552.
[15]
Dilles J H, Solomon G G, Taylor H P J, et al. 1992. Oxygen and hydrogen isotope characteristics of hydrothermal alteration at the Ann- Mason porphyry copper deposit, Yertington, Nevada[J]. Econ. Geol., 87: 44~63.
[16]
Drummond S E and Ohmoto H. 1985. Chemical evolution and mineral deposition in boiling hydrothermal sytems[J]. Econ. Geol., 80: 126~147.
[17]
Durr S B. 1996. Provenance of Xigaze fore-arc basin clastic rocks (Cretaceous, south Tibet) [J]. Geol. Soc. Am. Bull., 108: 669~684.
[18]
Eastoe, G G. 1978. A fluids inclusion study of the Panguna porphyry copper deposit, Bougainville, Papua New Guinea[J]. Econ. Geol., 73: 721~748.
[19]
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.
[20]
Harrison T M, Copeland P, Kidd W S F, et al. 1992. Raising Tibet[J]. Science, 255: 1663~1670.
[21]
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[22]
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.
[23]
Heinrich C A, Ryan C G, Mernagh T P, et al. 1992. Segregation of ore metals between magmatic brine and vapor: a fliud inclusion study using PIXE microanalysis[J]. Econ. Geol., 87: 1566~1583.
[24]
Hedenquist J W and Richards J P. 1998. The finfluence of geochemical techniques on the development of genetic models for porphyry copper deposits[J]. Rev. in Econ. Geol., 10: 235~256.
[25]
Hezarkhani A, Williams-Jones A E and Gammons C H. 1999. Factors controlling copper solubility and chalcopyrite deposition in the Sungun porphyry copper deposit, Iran[J]. Mineralium Deposita, 34: 770~783.
[26]
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]. Geology in China, 28: 27~29(in Chinese with English abstract).
[27]
Li Y Q, Rui Z Y ang Cheng L X. 1981. Fluid inclusions and mineralization of the Yulong porphyry copper (molybdenum) deposit[J]. Acta Geologica Sinia, 55(3): 216~312(in Chinese with English abstract).
[28]
Liu B and Shen K. 1999. Fliud inclusion thermodynamics[M]. Beijing: Geol. Pub. House (in Chinese with English abstract).
[29]
Mavrogenes J A, Bodnar R J, Anderson A J, et al. 1995. Assessment of the uncertainties and limitations of quantitative elemental analysis of individual fluid inclusion using synchrotron X-ray fluorescence(SXRF) [J]. Geochim. Cosmochim. Acta, 59: 3987~3995.
[30]
Meng X J, Hou Z Q, Gao Y F, et al. 2003. Re-Os dating for molybdenite from Qulong porphyry copper deposit in Gangdese metallogenic belt, Xizang and its metallogenic significance[J]. Geological Review, 49(6): 660~666(in Chinese with English abstract).
[31]
Nash J T. 1976. Fluid inclusion petrology data from porphyry copper deposits and application to exploration[A]. U.S. Geol. Survey Prof. Paper[C]. 907-D, 16.
[32]
Ni P, Rao B, Ding J Y, et al. 2003. Studies on the synthetic fluid inclusions and their application to Laser Raman spectrum analysis field[J]. Acta Petrologica Sinica, 19(2): 319~326(in Chinese with English abstract).
[33]
Qu X M, Hou Z Q, Huang W. 2001. Gangdese porphyry copper belt: the second Yulong porphyry copper belt in Tibrt[J]? Mineral Deposits, 20(4): 355~366(in Chinese with English abstract).
[34]
Roedder E. 1984. Fliud inclusion: reviews in mineralogy[J]. Mineralogical Society of America, 12: 644.
[35]
Rui Z Y, Huang C K, Qi G M, et al. 1984. Porphyry copper (molybdenum) deposits of China[M]. Beijing: Geol. Pub. House(in Chinese).
[36]
Schǎer U, Xu R H and All(e)re 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.
[37]
Sheets R W, Nesbitt B E and Muehlenbachs K. 1996. Meteoric water component in magmatic fluids from porphyry copper mineralization, Babine Lake area, British Columbia[J]. Geol., 24: 1091~1094.
[38]
Taylor H P J. 1974. The application of oxygen and hydrogen isotope studies to problems of hydrothermal alteration and ore deposition[J]. Econ. Geol., 60: 834~883.
[39]
Ulrich T, Günther D and Heinrich C A. 1999. Gold concentrations of magmatic brines and the metal budget of porphyry copper depoits[J]. Nature, 399: 676~679.
[40]
Ulrich T and Heinirich C A. 2001. Geology and alteration geochemistry of the porphyry Cu-Au deposit at Bajo de la Alumbrera Argentina[J]. Econ. Geol., 96: 1719~1742.
[41]
Var\'yash L N and Rekharskiy V I. 1981. Behaiour of Cu(I) in Chloritde solution[J]. Geochem. Int., 7: 1003~1008.
[42]
Wilson J W J, Kelser S E, Cloke P L, et al. 1980. Fluids inclusion geochemistry of the Granisle and Bell porphyry copper deposit, Bristish Columbia[J]. Econ. Geol., 75: 45~61.
[43]
Xu R H, Schǎer U and All(e)re C J. 1985. Magmatism and metamorphism in the Lhasa block(Tibet): a geochronological study[J]. J. Geol., 93: 41~57.
[44]
Yin A and Harrison T M. 2000. Geologic evolution of the Himalayan-Tibetan orogen[J]. Annu. Rev. Earth Planet. Sci., 28: 211~280.
[45]
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.
[46]
Zhang Q L, Qu X M, Xu W Y, et al. 2003. Study of the inclusions from Nanmu porphyry copper deposit in Tibet[J]. Acta Petrologica Sinica, 19(2): 251~259 (in Chinese with English abstract).
[47]
Zotov A V, Kudrin A V, Lein K A, et al. 1995. Experimental studies of the solubility and complexing of selected ore elements(Au,Ag,Cu,Mo,As,Sb,Hg) in aqueoue solutions[A]. In: Shmuloich K I, Yardley B W D, Gonchar G G, eds. Fliuds in the crust, equilibrium and transport properties[C]. London: Chapman and Hall. 95~132.