Frost D J,Wood B J.1997.Experimental measurements of the oxygen fugacity of CO2 and graphite/diamond stability from 35 to 77 kbar at 925 to 1650℃.Geochim.Cosmochim.Acta,61:1565～1574.
[37]
Kudo A M,Weill D F.1970.An igneous plagioclase thermometer.Contrib.Miner.Petro.,(25):52～65.
[38]
Naldrett A J.1999.World-class Ni-Cu-PGE deposits:Key factors in their genesis.Mineralium Deposita,34:227～240.
[39]
Toulmin P,Barton P B.1964.A thermodynamic study of pyrite and pyrrhotite.Geochimica et Cosmochimica Acta,28(5):641～671.
[40]
Wang Jingbin,WangG Yuwang,Wang Lijuan.2004.The Junggar Immature Continental Crust Province and Its Mineralization.Acta Geologica Sinica,78(2):337～344.
[41]
Wilemes J.1989.The geology of the Bushveld lgneous complex,the largest repository of magmatic ore deposits in the world.Economic Geology,4:966.
Boynton W V.1984.Cosmochemistry of the rare earth elements.Meteorite Studies Dev.Geochem.,2:63～114.
[49]
Fleet M E,Chryssoulis S L,Stone W E.1993.Partitioning of platinum-group elements and Au in the Fe-Ni-Cu-S system:experiments on the fractional crystallization of sulfide melt.Contributions to Mineralogy and Petrology,115:36～34.
[50]
Hess H H.1960.Stillwater igneous complex,Montana:a quantitative mineralogical study.Mem.Geol.Soc.Am.
[51]
Li C,Naldrett A J,Ripley E M.2001.Critical factors for the formation of a nickel-copper deposit in an evolved magma system:lessons from a comparison of the pants lake and Voisey\'s Bay sulfide occurrences in Labrador,Canada.Mineralium Deposita,36:85～92.
[52]
Shimazaki H,Naldrett A J.1975.Solubility of sulfur in an ultramafic melt and relevance of the system Fe-S-O.Econ.Geol.,70:960～967.
[53]
Vallace P J,Gerlach T M.1994.Magmatic vapor source for sulfur dioxide released during volcanic eruptions:evidence from Mount Pinatubo.Science,265:497～499.
[54]
Will G,Nover G.1979.Influence of oxygen partial pressure on the Mg/Fe distribution in olivine.Phys.Chem.Minerals,(4):199～208.
