W. Taylor

发表

The effect of fluorine on phase relationships in the system KAlSiO4-Mg2SiO4-SiO2 at 28 kbar and the solution mechanism of fluorine in silicate melts

D. Green, S. Foley, W. Taylor, 1986 .

Mantle-Derived Magmas - Roles of Variable Source Peridotite and Variable C-H-O Fluid Compositions

D. Green, T. Falloon, W. Taylor, 1987 .

The role of fluorine and oxygen fugacity in the genesis of the ultrapotassic rocks

D. Green, S. Foley, W. Taylor, 1986 .

An experimental test of some geothermometr and geobarometer formulations for upper mantle peridotites with application to the thermobarometry of fertile lherzolite and garnte websterite

W. Taylor, 1998 .

The liquidus surface of the system forsterite-nepheline-silica at 28 kb

D. Green, W. Taylor, Alok K. Gupta, 1987 .

The role of C-O-H fluids in upper mantle processes : a theoretical, experimental and spectroscopic study

W. Taylor, 1985 .

Carbon isotopic fractionation between CO2 vapour, silicate and carbonate melts: an experimental study to 30 kbar

C. Pillinger, D. Green, D. Mattey, 1990 .

The Earth's upper mantle as a source for volatiles

D. Green, S. Foley, W. Taylor, 1990 .