Morales Ruano, S, Both, R.A, Golding, S.D (2002) A fluid inclusion and stable isotope study of the Moonta copper–gold deposits, South Australia: evidence for fluid immiscibility in a magmatic hydrothermal system. Chemical Geology, 192 (3) 211-226 doi:10.1016/s0009-2541(02)00197-3

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See Also

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	Morales-Ruano, S., Both, R.A., Golding, S.D. (2002) A fluid inclusion and stable isotope study of the Moonta copper-gold deposits, South Australia: evidence for fluid immiscibility in a magmatic hydrothermal system. Chemical Geology, Vol. 192, pg. 211-226.
	Moore, Joseph N, Norman, David I, Kennedy, B.Mack (2001) Fluid inclusion gas compositions from an active magmatic–hydrothermal system: a case study of The Geysers geothermal field, USA. Chemical Geology, 173 (1) 3-30 doi:10.1016/s0009-2541(00)00265-5
	Polito, P. A., Kyser, T. K., Golding, S. D., Southgate, P. N. (2006) Zinc Deposits and Related Mineralization of the Burketown Mineral Field, Including the World-Class Century Deposit, Northern Australia: Fluid Inclusion and Stable Isotope Evidence for Basin Fluid Sources. Economic Geology, 101 (6) 1251-1273 doi:10.2113/gsecongeo.101.6.1251
	Simon, Klaus (2001) Does δD from fluid inclusion in quartz reflect the original hydrothermal fluid?. Chemical Geology, 177 (3) 483-495 doi:10.1016/s0009-2541(00)00417-4
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	Harris, A. C., Golding, S. D., White, N. C. (2005) Bajo de la Alumbrera Copper-Gold Deposit: Stable Isotope Evidence for a Porphyry-Related Hydrothermal System Dominated by Magmatic Aqueous Fluids. Economic Geology, 100 (5), 863-886. doi:10.2113/gsecongeo.100.5.863
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	Dugdale, A.L., Hagemann, S.G. (2001) The Bronzewing lode-gold deposit, Western Australia: P–T–X evidence for fluid immiscibility caused by cyclic decompression in gold-bearing quartz-veins. Chemical Geology, 173 (1) 59-90 doi:10.1016/s0009-2541(00)00268-0
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	Bethke, P.M., Ryeb, R.O., Stoffregen, R.E., and Vikre, P.G. (2005). Evolution of the magmatic-hydrothermal acid-sulfate system at Summitville, Colorado: integration of geological, stable isotope, and fluid-inclusion evidence. Chemical Geology: 215: 281–315.
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