Calculation of magmatic fluid contributions to porphyry-type ore systems: Predicting fluid inclusion chemistries. release_aliimd55org2db2q46imr4532y

by Philip A. Candela

References

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Beane, R. E. and Titley, S. R. (1981) Porphyry copper deposits: Part II. Hydrothermal alteration and mineralization. Econ. Geol. 75, 235-269.
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Brandeis, G. and Jaupart, C. (1987), Crystal sizes in intrusions of different dimensions: constraints on the cooling regieme and the crystallization kinetics, Magmatic Processes: Physiochemical Principles, Mysen, B. 0., ed., (The Geochemical Society, Special Publication 1) 307-318.
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Candela, P. A. (1982) Copper and Molybdenum is silicate met-aqueous fluid systems; Ph. D. Thesis, Harvard University, Cambridge, Massachusetts, 138p.
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Candela, P. A. (1986) Generalizaed mathematical modes for the fractional evolution of vapor from magmas in terrestrial planetary crusts; Advances in Physical Geochemistry, 6, Saxena, S. K., ed., New York, Springer-Verlag 362-396.
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London, D. Morgan, G. B., VI and Hervig, R. L. (1989) Vapor-undersaturated experiments with
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Macusani glass + H20 at 200 MPa, and the internal differentiation of granitic pegmatites. Contrib. Mineral. Petrol. 102, 1-17.
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Marsh, B. D. (1981) On the Crystallinity, Probability of Occurrence, and Rheology of Lava and Magma. Contrib. Mineral. Petrol. 78, 85-98.
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Chemical composition of the hydrothermal fluids responsible for the lead-zinc deposits at Providencia, Zacatecas, Mexico
Robert O. Rye, Joseph Haffty
1969   Economic Geology and The Bulletin of the Society of Economic Geologists
doi:10.2113/gsecongeo.64.6.629 
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E., Jr. (1985) Geologic, fluid inclusion, and geochemical studies of the mineralized breccias at Cumobabi, Sonora, Mexico. Econ. Geol. 80, 1566 1592.
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Shinohara, H., Iiyama, T. and Matsuo, S. (1984) Comportement du chlore dans le systeme magma granitique-eau: C. R. Acad. Sc. Paris, 298, Serie II, n° 17, 741.
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Tacker, R. C. and Candela, P. A., (1987) Partitioning of molybdenum between magnetite and melt: a preliminary study of the partitioning of ore metals between silicic magmas and crystalline phases. Econ. Geol. 82, 1827-1838.
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Urabe, T. (1985) Aluminous granite as a source of hydrothermal ore-deposits: an experiments study. Econ. Geol. 80, 148-157.
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The effect of pressure on the partitioning ratios of lead and zinc between vapor and rhyolite melts
Tetsuro Urabe
1987   Economic Geology and The Bulletin of the Society of Economic Geologists
doi:10.2113/gsecongeo.82.4.1049 
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Webster, J. D., Holloway, J. R. and Hervig, R. L. (1988) Partitioning of lithophile trace elements be tween H20 and H20 + CO2 fluids and topaz ryholite melt. Econ. Geol. 84, 116-134.