Pórfidos Cupríferos

Génesis de Pórfidos Cupríferos 25
Geochimica et Cosmochimica Acta, v. 49, p. 1861-
1873.
Bowen, N.L., 1933, The broader story of magmatic
differentiation, briefly told, in Ore deposits of the
Western States (Lindgren volume): American
Institute of Mining and Metallurgical Engineers, p.
106-128.
Bowman, J.R., Parry, W.T., Kropp, W.P., and Kruer, S.A.,
1987, Chemical and isotopic evolution of
hydrothermal solutions at Bingham, Utah: Economic
Geology, v. 82, p. 395-428.
Brimhall, G. H, Jr., 1980, Deep hypogene oxidation of
porphyry copper potassium-silicate protore at Butte,
Montana, a theoretical evaluation of the copper
remobilization hypothesis: Economic Geology, v. 75,
p. 384-409.
Burnham, C.W., 1967, Hydrothermal fluids at the
magmatic stage, in Barnes, H.L., ed., Geochemistry
of hydrothermal ore deposits: New York, Holt,
Rinehart and Winston, p. 34-76.
____________, 1979, Magmas and hydrothermal fluids, in
Barnes, H.L., ed., Geochemistry of hydrothermal ore
deposits, 2nd edition: New York, John Wiley, p. 71-
136.
Burnham, C.W., and Jahns, R.H., 1962, A method for
determining the solubility of water in silicate melts:
American Journal of Science, v. 260, p. 721-745.
Burnham, C.W., and Ohmoto, H., 1980, Late-stage
processes in felsic magmatism: Mining Geology
Special Issue, No. 8, p. 1-11.
Candela, P.A., 1989, Magmatic ore-forming fluids:
thermodynamic and mass transfer calculations of
metal concentrations: Reviews in Economic Geology,
v. 4, p. 223-233.
Carten, R.B., White, W.H., and Stein, H J., 1993, Highgrade
granite related molybdenum systems:
Geological Association of Canada, Special Paper 40,
p. 521-554.
Cathles, L.M., II, 1977, An analysis of the cooling of
intrusives by groundwater convection that includes
boiling: Economic Geology, v. 72, p. 804-826.
Cathles, L.M., 1981. Fluid flow and genesis of
hydrothermal ore deposits. Economic Geology 75th
Anniversary Volume, p. 424-457.
Cathles, L.M., 1997. Thermal Aspects of Ore Formation.
In: Barnes, H.Ll. (Editor) Geochemistry of
Hydrothermal Ore Deposits, Third Edition, John
Willey & Sons, p. 191-223.
Cathles, L.M.; Erendi, A.H.J.; Thayer, J.B., and Barrie, T.,
1997. How long can a hydrothermal system be
sustained by a single intrusion event?. Economic
Geology, V. 92, Nº 7/8, pp. 766-771
Chivas, A.R., and McDougall, I., 1978, Geochronology of
the Koloula porphyry copper prospect, Guadalcanal,
Solomon Islands: Economic Geology, v. 73, p. 678-
679.
Clark, A.H., 1993. Are outsize porphyry copper deposits
either anatomically or environmentally distinctive?:
Society of Economic Geologists Special Publication,
no. 2, p. 213-283.
Clark, A.H., Archibald, D.A , Lee, A.W., Farrar, E., and
Hodgson, C.J., 1998, Laser-probe 40Ar-39Ar ages of
early- and late-stage alteration assemblages, Rosario
porphyry copper-molybdenum deposit, Collahuasi
District, I Region, Chile: Economic Geology, v. 93,
p. 326-337.
Cline, J.S., 1995, Genesis of porphyry copper deposits: the
behavior of water, chloride, and copper in
crystallizing melts, in Pierce, EW., and Bolm, J.G.,
eds., Porphyry copper deposits of the American
Cordillera: Arizona Geological Society Digest, v. 20,
p. 69-82.
Cline, J.S., and Bodnar, R J., 1991, Can economic porphyry
copper mineralization be generated by a typical calcalkaline
melt?: Journal of Geophysical Research, v.
96, p. 8113-8126.
Cline, J.S., and Vanko, D.A., 1995, Magmatically
generated saline brines related to molybdenum at
Questa, New Mexico, in Thompson, J.E.H., ed.,
Magmas, fluids, and ore deposits: Mineralogical
Association of Canada Short Course, v. 23, p. 153-
174.
Cornejo, P., Tosdal, R.M., Mpodozis, G., Tomlinson, A.J.,
Rivera, O., and Fanning, C.M., 1997, El Salvador,
Chile porphyry copper deposit revisited: geologic and
geochronologic framework: International Geology
Review, v. 39, p. 22-54.
Craig, H., Boato, G., and White, D.E., 1956, The isotopic
geochemistry of thermal waters: National Research
Council Nuclear Sciences Series, Report 19, p. 29-
44.
Creasey, S.C., 1966, Hydrothermal alteration, in Titley,
S.R., and Hicks, C.L., eds., Geology of the porphyry
copper deposits-southwestern North America:
Tucson, University of Arizona Press, p. 51-74.
Dilles, J.H., 1987, Petrology of the Yerington batholith,
Nevada: Evidence for evolution of porphyry copper
ore fluids: Economic Geology, v. 82, p. 1750-1789.
Dilles, J.H., and Proffett, J.M, 1995, Metallogenesis of the
Yerington batholith, Nevada, in Pierce, EW., and
Bolm, J.G., eds., Porphyry copper deposits of the
American Cordillera: Arizona Geological Society
Digest, v. 20, p. 306-315.
Dilles, J.H., Solomon, G.C., Taylor, H.P., Jr., and Einaudi,
M.T, 1992, Oxygen and hydrogen isotope
characteristics of hydrothermal alteration at the Ann-
Mason porphyry copper deposit, Yerington, Nevada:
Economic Geology, v. 87, p. 44-63.
Dobson, P.F., Epstein, S. and Stolper, E.M., 1989,
Hydrogen isotope fractionation between coexisting
vapor and silicate glasses and melts at low pressure:
Geochimica et Cosmochimica Acta, v. 53, p. 2723-
2730.
Doe, B.R., and Zartman, R.E., 1979, Plumbotectonics, the
Phanerozoic, in Barnes, H.L., ed., Geochemistry of
hydrothermal ore deposits, 2nd edition: New York,
John Wiley, p. 22-70.
Eastoe, C.J., 1978, A fluid inclusion study of the Panguna
porphyry copper deposit, Bougainville, Papua New
Guinea: Economic Geology, v. 73, p. 721-748.
Einaudi, M.T, 1982, Description of skarns associated with
porphyry copper plutons-southwestern North
America, in Titley, S.R., ed., Advances in geology of
the porphyry copper deposits-southwestern North