Arnold, G. O. & Sillitoe, R. H. 1989. Mount Morgan gold–copper deposit, Queensland, Australia: evidence for an intrusion-related replacement origin. ECON GEOL 84, 1805–16.
Baker, E. M. & Andrew, A. S. 1991. Geologic, fluid inclusion, and stable isotope studies of the gold bearing breccia pipe at Kidston, Queensland, Australia. ECON GEOL 86, 810–30.
Burnham, C. W.1979.Magmas and hydrothermal fluids. InBarnes, H. L. (ed.) Geochemistry of hydrothermal ore deposits (2nd edn), 71–136. New York: Wiley.
Burnham, C. W. & Ohmoto, H. 1980. Late-stage processes of felsic magmatism. In Ishihara, S. & Takenouchi, S. (eds) Granite magmatism and related mineralisation. MIN GEOL SPEC ISSUE 8, 1–11.
Candela, P. A. 1989. Felsic magmas, volatile, and metallogenesis. SOC ECON GEOL REV ECON GEOL 4, 223–33.
Candela, P. A. & Bouton, S. L. 1990. The influence of oxygen fugacity on tungsten and molybdenum partitioning between silicate melts and ilmenite. ECON GEOL 85, 633–40.
Candela, P. A. & Holland, H. D. 1986. A mass transfer model for copper and molybdenum in magmatic hydrothermal systems: The origin of porphyry-type ore deposits. ECON GEOL 81, 1–19.
Carmichael, I. S. E. 1991. The redox state of basic and silicic magmas: a reflection of their source regions? CONTRIB MINERAL PETROL 106, 129–41.
Carroll, M. R. & Rutherford, M. J. 1985. Sulphide and sulphate saturation in hydrous silicate melts. J GEOPHYS RES 90, C601–12.
Chappell, B. W. 1984. Source rocks of I- and S-type granites in the Lachlan Fold Belt, southeastern Australia. PHILOS TRANS R SOC LONDON A310, 693–707.
Chappell, B. W. & Stephens, W. E. 1988. Origin of infracrustal (I-type) granite magmas. TRANS R SOC EDINBURGH EARTH SCI 79, 71–86.
Chappell, B. W. & White, A. J. R. 1984. I- and S-type granites in the Lachlan Fold Belt, southeastern Australia. In Keqin, Xu & Guanchi, Tu (eds) Geology of granites and their metallogenic relations, 87–101. Beijing: Science Press.
Chappell, B. W. & White, A. J. R. 1992. I-type and S-type granites in the Lachlan Fold Belt. TRANS R SOC EDINBURGH EARTH SCI 83, 1–26.
Chappell, B. W., White, A. J. R. & Wyborn, D. 1987. The importance of residual source material (restite) in granite petrogenesis. J PETROL 28, 1111–38.
Chappell, B. W., White, A. J. R. & Hine, R. 1988. Granite provinces and basement terranes in the Lachlan Fold Belt, southeastern Australia. AUST J EARTH SCI 35, 505–21.
Chappell, B. W., Wyborn, L. A. I., White, A. J. R., Burnham, C. W. & Wyborn, D. (in prep.). S-type granites of the Wagga Basement Terrane: an example of compositional variation resulting from sequential restite fractionation, fractional crystallisation, and hydrothermal alteration.
Cochrane, G. W. 1971. Tin deposits of Victoria. GEOL SURV VICTORIA BULL 60.
Collins, W. J., Beams, S. D., White, A. J. R. & Chappell, B. W. 1982. Nature and origin of A-type granites with particular reference to southeastern Australia. CONTRIB MINERAL PETROL 80, 189–200.
Einaudi, M. T., Meinert, L. D. & Newberry, R. J. 1981. Skarn deposits. ECON GEOL 75TH ANNIVERSARY VOL 317–91.
Flood, R. H. & Shaw, S. E. 1975. A cordierite-bearing granite suite from the New England Batholith, NSW. CONTRIB MINERAL PETROL 52, 157–64.
Haughton, D. R., Roeder, P. L. & Skinner, B. J. 1974. Solubility of sulphur in mafic magmas. ECON GEOL 69, 451–67.
Heinrich, C. A. 1990. The chemistry of hydrothermal tin (–tungsten) ore deposition. ECON GEOL 85, 457–81.
Hine, R., Williams, I. S. & Chappell, B. W. 1978. Contrasts between I- and S-type granitoids of the Kosciusko Batholith. J GEOL SOC AUST 25, 219–34.
Horton, D. J. 1978. Porphyry-type copper-molybdenum mineralisation belts in eastern Queensland. ECON GEOL 73, 904–21.
Ishihara, S. 1981. The granitoid series and mineralisation. ECON GEOL 75TH ANNIVERSARY VOL, 458–84.
Ivanova, G. F. & Butuzova, Ye. G. 1968. Distribution of tungsten, tin and molybdenum in granites of eastern Transbaikalia. GEOKHIMIY A 6, 689–700.
Jaireth, S., Heinrich, C. A. & Solomon, M. 1990. Chemical controls on hydrothermal tungsten transport and the precipitation of ferberite and scheelite. GEOL SOC AUST ABSTR 25, 269–70.
Katsura, T. & Nagashima, S. 1974. Solubility of sulphur in some magmas at 1 atmosphere. GEOCHIM COSMOCHIM ACTA 38, 517–31.
Keith, J. D., van Middelaar, W., Clark, A. H. & Hodgson, C. J. 1989. Granitoid textures, compositions, and volatile fugacities associated with the formation of tungsten-dominated skarn deposits. SOC ECON GEOL REV ECON GEOL 4, 235–50.
Kilinc, I. A. & Burnham, C. W. 1972. Partitioning of chloride between a silicate melt and coexisting aqueous phase from 2 to 8 kilobars. ECON GEOL 67, 231–5.
Kwak, T. A. P. 1987. W-Sn skarn deposits and related metamorphic skarns and granitoids. Amsterdam: Elsevier.
Lehmann, B. 1990. Metallogeny of Tin. Berlin: Springer.
Loiselle, M. C. & Wones, D. R. 1979. Characteristics and origin of anorogenic granites. GEOL SOC AM ABSTR PROG 11, 468.
Lynton, S. J., Candela, P. A. & Piccoli, P. M. 1990. Experimental determination of copper partitioning between pyrrhotite and high silica rhyolite. GEOL SOC AM ABSTR PROG 22, 181.
Markham, N. L. & Basden, H. 1974. The mineral deposits of New South Wales. Sydney: Geological Survey of New South Wales.
Munoz, J. L. 1984. F-OH and Cl-OH exchange in micas with applications to hydrothermal ore deposits. MIN SOC AM REV MINERAL 13, 469–93.
Murray, C. G. 1990. Tasman Fold Belt in Queensland. In Hughes, F. E. (ed.) Geology of the mineral deposits of Australia and Papua New Guinea, 1431–50. Melbourne: Australasian Institute of Mining and Metallurgy.
Newberry, R. J. & Swanson, S. E. 1986. Scheelite skarn granitoids: an evaluation of the roles of magmatic source and process. ORE GEOL REV 1, 57–81.
Newberry, R. J., Burns, L. E., Swanson, S. E. & Smith, T. E. 1990. Comparative petrologic evolution of the Sn and W granites of the Fairbanks-Circle area, interior Alaska. In Stein, H. J. & Hannah, J. L. (eds) Ore-bearing granite systems: petrogenesis and mineralising processes. PROF PAP US GEOL SURV 246, 121–42.
Plimer, I. R. 1980. Exhalative tin and tungsten deposits associated with mafic volcanism as precursors to tin and tungsten deposits associated with granites. MINER DEPOSITA 15, 275–89.
Stanton, R. L. 1972. Ore petrology. New York: McGraw-Hill.
Stanton, R. L. 1990. Magmatic evolution and the ore type-lava type affiliations of volcanic exhalative ores. In Hughes, F. E. (ed.) Geology of the mineral deposits of Australia and Papua New Guinea, 101–7. Melbourne: Australian Institute of Mining and Metallurgy.
Tacker, R. C. & Candela, P. A. 1987. Partitioning of molybdenum between magnetite and melt: a preliminary study of the partitioning between silicic magmas and crystalline phases. ECON GEOL 82, 1827–38.
Taylor, J. R. & Wall, V. J. 1990. The behaviour of tin in magmatic-hydrothermal systems. GEOL SOC AUST ABSTR 25, 270–1.
Turner, N. J. & Taheri, J. 1990. Tin and tungsten deposits and related Devonian granitoids. Excursion Guide E2, 10th Australian Geological Convention, Geological Society of Australia.
van Middelaar, W. T. & Keith, J. D. 1990. Mica cheimstry as an indicator of oxygen and halogen fugacities in the CanTung and other W-related granitoids in the North American Cordillera. In Stein, H. J. & Hannah, J. L. (eds) Ore-bearing granite systems; petrogenesis and mineralising processes. GEOL SOC AM PROF PAP 246, 205–20.
Watchhorn, R. B. & Wilson, C. J. L. 1989. Structural setting of the gold mineralization at Stawell, Victoria, Australia. In Keays, R. R., Ramsay, W. R. H. & Groves, D. I. (eds) The geology of gold deposits: The perspective in 1988. ECON GEOL MONOGR 6, 292–309.
Weber, C. R., Paterson, I. B. L. & Townsend, D. J. 1978. Molybdenum in New South Wales. GEOL SURV NEW SOUTH WALES MIN RES 43.
Wesolowski, D., Cramer, J. & Ohmoto, H. 1988. Scheelite mineralsiation in skarns adjacent to Devonian granitoids at King Island, Tasmania. In Taylor, R. P. & Strong, D. F. (eds) Recent Advances in the Geology of Granite-Related Mineral Deposits. CAN INST MIN METALL SPEC VOL 39, 234–51.
Whalen, J. B. & Chappell, B. W. 1988. Opaque mineralogy and mafic mineral chemistry of I- and S-type granites of the Lachlan Fold Belt, southeast Australia. AM MINERAL 73, 281–96.
White, A. J. R. & Chappell, B. W. 1977. Ultrametamorphism and granitoid genesis. TECTONOPHYSICS 43, 7–22.
White, A. J. R. & Chappell, B. W. 1988. Some supracrustal (S-type) granites of the Lachlan Fold Belt. TRANS R SOC EDINBURGH EARTH SCI 79, 169–81.
Williams, E., McClenaghan, M. P. & Collins, P. L. F. 1989. Mid-Palaeozoic deformation, granitoids and ore deposits. In Burrett, C. F. & Martin, E. L. (eds) Geology and Mineral Resources of Tasmania. GEOL SOC AUST SPEC PUBL 15, 238–92.
Wood, S. A. & Vlassopoulos, D. 1989. Experimental determination of the hydrothermal solubility and speciation of tungsten at 500°C and 1 kbar. GEOCHIM COSMOCHIM ACTA 53, 303–12.
Wyborn, D., Turner, B. S. & Chappell, B. W. 1987. The Boggy Plain Supersuite: a distinctive belt of I-type igneous rocks of potential economic significance in the Lachlan Fold Belt. AUST J EARTH SCI 34, 21–43.