Exsolution of magmatic volatile phases from Cl-enriched mineralizing granitic magmas and implications for ore metal transport

[1]  D. Burt,et al.  Volatile and lithophile trace-element geochemistry of Mexican tin rhyolite magmas deduced from melt inclusions , 1996 .

[2]  John R. Holloway,et al.  Application of experimental results to C-O-H species in natural melts , 1994 .

[3]  J. Webster,et al.  Solubilities of sulfur, noble gases, nitrogen, chlorine, and fluorine in magmas , 1994 .

[4]  H. Shinohara.  Exsolution of immiscible vapor and liquid phases from a crystallizing silicate melt: Implications for chlorine and metal transport , 1994 .

[5]  H. Keppler,et al.  Distribution of chloride between aqueous fluids and felsic melts at 2 kbar and 800°C , 1994 .

[6]  W. Duffield,et al.  Extreme halogen abundances in tin-rich magma of the Taylor Creek Rhyolite, New Mexico , 1994 .

[7]  H. Palme,et al.  The effect of oxygen fugacity and temperature on solubilities of nickel, cobalt, and molybdenum in silicate melts , 1994 .

[8]  A. T. Anderson,et al.  Diffusive reequilibration of melt and fluid inclusions , 1992 .

[9]  J. Webster.  Fluid-melt interactions involving Cl-rich granites: Experimental study from 2 to 8 kbar , 1992 .

[10]  J. Webster.  Water solubility and chlorine partitioning in Cl-rich granitic systems: Effects of melt composition at 2 kbar and 800°C , 1992 .

[11]  D. Dingwell,et al.  FLUORINE IN SILICATE GLASSES : A MULTINUCLEAR NUCLEAR MAGNETIC RESONANCE STUDY , 1992 .

[12]  H. Keppler,et al.  Partitioning of Cu, Sn, Mo, W, U, and Th between melt and aqueous fluid in the systems haplogranite-H2O−HCl and haplogranite-H2O−HF , 1991 .

[13]  W. Duffield,et al.  Volatiles and lithophile elements in Taylor Creek Rhyolite; constraints from glass inclusion analysis , 1991 .

[14]  R. Bodnar,et al.  Can economic porphyry copper mineralization be generated by a typical calc‐alkaline melt? , 1991 .

[15]  S. Kohn,et al.  NMR evidence for five- and six-coordinated aluminum fluoride complexes in F-bearing aluminosilicate glasses , 1991 .

[16]  P. Candela,et al.  The influence of oxygen fugacity on tungsten and molybdenum partitioning between silicate melts and ilmenite , 1990 .

[17]  H. Shinohara,et al.  Partition of chlorine compounds between silicate melt and hydrothermal solutions: I. Partition of NaCl-KCl , 1989 .

[18]  J. Webster,et al.  Partitioning of lithophile trace elements between H 2 O and H 2 O + CO 2 fluids and topaz rhyolite melt , 1989 .

[19]  B. M. Walker,et al.  Cyclic development of igneous features and their relationship to high-temperature hydrothermal features in the Henderson porphyry molybdenum deposit, Colorado , 1988 .

[20]  M. McCulloch,et al.  Sm-Nd isotope systematics in uranium rare-earth element mineralization at the Mary Kathleen uranium mine, Queensland , 1987 .

[21]  P. Candela,et al.  Partitioning of molybdenum between magnetite and melt; a preliminary experimental study of partitioning of ore metals between silicic magmas and crystalline phases , 1987 .

[22]  I. Chou.  Phase relations in the system NaCl-KCl-H2O. III: Solubilities of halite in vapor-saturated liquids above 445°C and redetermination of phase equilibrium properties in the system NaCl-H2O to 1000°C and 1500 bars , 1987 .

[23]  B. Mysen,et al.  Structure and properties of fluorine-bearing aluminosilicate melts: the system Na2O-Al2O3-SiO2-F at 1 atm , 1985 .

[24]  R. Bodnar,et al.  Synthetic fluid inclusions in natural quartz. III. Determination of phase equilibrium properties in the system H2O-NaCl to 1000°C and 1500 bars , 1985 .

[25]  H. D. Holland,et al.  The partitioning of copper and molybdenum between silicate melts and aqueous fluids , 1984 .

[26]  W. Giggenbach.  Book reviewChemistry and geochemistry of solutions at high temperatures and pressures: Editors D. T. Rickard and F. E. Wickman, Pergamon Press, 1981, 564 pages, US$170 , 1983 .

[27]  E. Christiansen,et al.  Topaz rhyolites; distribution, origin, and significance for exploration , 1982 .

[28]  D. Manning,et al.  The probable occurrence of interstitial Al in hydrous, F-bearing and F-free aluminosilicate melts , 1981 .

[29]  D. A. Johnston.  Volcanic Contribution of Chlorine to the Stratosphere: More Significant to Ozone Than Previously Estimated? , 1980, Science.

[30]  S. C. Creasey.  Intrusives associated with porphyry copper deposits , 1977 .

[31]  J. Holloway.  Fluids in the evolution of granitic magmas: Consequences of finite CO2 solubility , 1976 .

[32]  A. K. V. Groos,et al.  Melting Relationships in the System NaAlSi3O8-NaCl-H2O at One Kilobar Pressure, with Petrological Applications , 1969, The Journal of Geology.

[33]  G. Kennedy,et al.  THE SYSTEM H$sub 2$O-NaCl AT ELEVATED TEMPERATURES AND PRESSURES , 1960 .

[34]  J. F. Thompson.  Magmas, fluids, and ore deposits , 1995 .

[35]  John R. Holloway,et al.  Volatiles in magmas , 1994 .

[36]  E. Christiansen,et al.  The genesis of giant porphyry molybdenum deposits , 1993 .

[37]  D. Dingwell,et al.  Effects of F, B2O3 and P2O5 on the solubility of water in haplogranite melts compared to natural silicate melts , 1993 .

[38]  C. Hodgson,et al.  Giant Ore Deposits , 1993 .

[39]  E. Roedder.  Fluid inclusion evidence for immiscibility in magmatic differentiation , 1992 .

[40]  C. S. Hutchison.  Economic deposits and their tectonic setting , 1983 .

[41]  C. Burnham.  The nature of multicomponent aluminosilicate melts , 1981 .

[42]  J. Hunt,et al.  Porphyry copper deposits , 1977, Geological Society, London, Special Publications.

[43]  H. Barnes,et al.  Geochemistry of Hydrothermal Ore Deposits , 1968 .