［1］Arnold R,Gordon C and LloydC.1995.Geology and mining of Nevoria gold mine[A].In:Schwebel PJ,ed..Southern CrossGreenstone Belt,Geology and Gold Mines:Southern Cross,Western Australia[C].GeoconferenceExtended Abstract.97～101.
[2]
［2］Bakker R J.1997.Clathrates:Computer programs to calculate fluid inclusion V-Xproperties using clathrate melting temperatures[J].Computers & Geosciences,23:1～18.
[3]
［3］Bouchot V,Fan H R,Vanderhor F,et al.1996.Temporal relationships between barrencalc-silicate and auriferous quartz-sulphide veins at the Nevoria gold deposit,YilgarnBlock,Australia:Evidence for both pre- and post-peak metamorphic hydrothermalevents[A].Abstract of 30th International Geological Congress[C],Beijing,2:760p.
[4]
［4］Brown P E,Hagemann S G.1995.MacFlincor and its application to fluids in Archeanlode-gold deposits[J].Geochimica et Cosmochimica Acta,59:3943～3952.
[5]
［5］Cullen I,Jones M and Baxter J L.1990.Nevoria gold deposits[A].In:HugherFE,ed..Geology of the Mineral deposits of Australia and Papua New Guinea[C].The AustralianInstitute of Mining and Metallurgy,Melbourne,301～305.
[6]
［6］Gee R D.1995.Regional geology of the Southern Cross greenstone belt[A].in SchwebelPJ,ed..Southern Cross Greenstone Belt,Geology and Gold Mines[C].Southern Cross,WesternAustralia Geoconference Extended Abstract.11～16.
[7]
［7］Groves D I.1993.The Crustal continuum model for late-Archaean lode-gold deposits ofthe Yilgarn Block,Western Australia[J].Mineralium Deposita,28:366～374.
[8]
［8］Groves D I,Goldfarb R J,Knox-Robinson C M,et al.2000.Late-kinematic timing oforogenic gold deposits and significance for computer-based exploration techniques withemphasis on the Yilgarn Block,Western Australia[J].Ore Geology Reviews,17:1～38.
[9]
［9］Ho S E,Groves D I,McNaughton N J,et al.1992.The source of ore fluid and solutes inArchaean lode-gold deposits of Western Australia[J].Journal of Volcanic and GeothermalResearch,50:173～196.
[10]
［10］Hollister L S,Burruss R C.1976.Phase equilibria in fluid inclusions from theKhtada metamorphic complex[J].Geochimica et Cosmochimica Acta,40:163～175.
[11]
［11］Mernagh T P,Witt W K.1994.Early methane-rich fluids and their role in Archean goldmineralisation at the Sand King and Missouri deposits,Eastern Goldfields Province,WesternAustralia[J].AGSO Journal of Australia Geology and Geophysics.15:297～312.
[12]
［12］Mullis J.1987.Fluid inclusion studies during very low-grademetamorphism[A].In:Frey M,ed.,Low Temperature Metamorphism[M].Blackie:Glasgow,162～199.
[13]
［13］Ramboz C,Schnapper D,Dubessy J.1985.The P-V-T-X-fO2 evolution of H2O-CH4-CO2-bearingfluid in a wolframite vein,Reconstruction from fluid inclusion studies[J].Geochimica etCosmochimica Acta,49:205～219.
[14]
［14］Ridley J,Hagemann S G.1999.Interpretation of post-entrapment fluid-inclusionre-equilibration at the Three Hill,Marvel Loch and Griffins Find high-temperaturelode-gold deposits,Yilgarn Black,Western Australia[J].Chem.Geol.,154:257～278.
