Bodnar R J. 1993. Revised equation and table for determining the freezing point depression of H2O-NaCl solutions. Geochimica Cosmochimica Acta, 57(3): 683-684.
[27]
Brown P E and Lamb W M. 1989. P-V-T properties of fluids in the system H2O±CO2±NaCl: New graphic presentations and implications for fluid inclusion studies. Geochim Cosmochim Acta, 53: 1209-1221.
[28]
Chai F M, Mao J, Dong L H, Yang F Q, Liu F, Geng X X and Zhang Z X. 2009. Geochronology of metarhyolites from the Kangbutiebao Formation in the Kelang basin, Altay Mountains, Xinjiang: Implications for the tectonic evolution and metallogeny. Gondwana Research, 16, 189-200.
[29]
Chen Y J, Pirajno F and Sui Y H. 2004. Isotope geochemistry of the Tieluping silver deposit, Henan, China: A case study of orogenic silver deposits and related tectonic setting. Mineralium Deposita, 39: 560-575.
[30]
Chen Y J, Sui Y H and Gao X L. 2001. Fluid geochemistry of Tieluping Ag ore and its implications for the CPMF model // Water-Rock Interaction 2001, Swets &Zeitltinger, Lisse: 689-692.
[31]
Collins P L F. 1979. Gas hydrates in CO2-bearing fluid inclusions and use freezing data for estimation of salinity. Economic Geology, 74: 1435-1444.
[32]
Groves D I, Goldfarb R J, Gebre-Mariam M, Hagemann S G and Robert F. 1998. Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Reviews, 13: 7-27.
[33]
Kerrich R, Goldfarb R, Groves D, Garwin S and Jia Y. 2000. The characteristics, origins, and geodynamic settings of supergiant gold metallogenic provinces. Science in China Series D-Earth Sciences, 43(supp): 1-68.
[34]
Kreuzer O P. 2005. Intrusion-hosted mineralization in the charters towers goldfield, North Queensland: New isotopic and fluid inclusion constraints on the timing and origin of the auriferous veins. Economic Geology, 100(8): 1583-1603.
[35]
Sengor A M C and Natal''in B A. 1996. Paleotectonics of Asia: Frangments of synthesis // Yin A and Harrison T M. The Tectonic Evolution of Asia. Cambridge: Cambridge University Press: 480-640.
[36]
Sibson R H, Robert F and Poulsen K H. 1988. High-angle reverse faults,fluid-pressure cycling,and mesothermal gold deposits. Geology, 16: 551-555.
[37]
Sun M, Yuan C, Xiao W J, Long X P, Xia X P, Zhao G C, Lin S F, Wu F Y and Kroner A. 2008. Zircon U-Pb and Hf isotope study of gneissic rocks from Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic. Chemical Geology, 247: 352-383.
[38]
Wan B, Zhang L C and Xiao W J. 2010. Geological and Geochemical characteristics and ore genesis of Keketale Pb-Zn deposit, Southern Altay Metallogenic Belt, NW China. Ore Geology Review, 37: 114-126.
[39]
Xiao W J, Pirajno F and Seltmann R. 2008. Geodynamics and metallogeny of the Altaid orogen. Journal of Asian Earth Sciences, 32(2-4): 77-81.
[40]
Xiao W J, Windley B F and Hao J. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of Central Asian orogenic belt. Tectonics, 22: 1069.
[41]
Xiao W J, Windley B F, Huang B C, Han C M, Yuan C, Chen H L, Sun M, Sun S and Li J L. 2009. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: Implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia. International Journal of Earth Sciences, 98(6): 1189-1217.
