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Scott Wood, D. Crerar, M. Borcsik (1987)
Solubility of the assemblage pyrite-pyrrhotite-magnetite-sphalerite-galena-gold-stibnite-bismuthinite-argen- tite-molybdenite in H 2 O-NaCl-CO 2 solutions from 200 degrees to 350 degrees C degreesEconomic Geology, 82
C. Gammons, H. Barnes (1989)
The solubility of Ag2S in near-neutral aqueous sulfide solutions at 25 to 300°C☆Geochimica et Cosmochimica Acta, 53
Wood Wood, Creraar Creraar, Brocsik Brocsik (1987)
Solubility of the assemblage pyritepyrrhotite‐ magnetite sphalerite‐galena‐gold‐stibnite‐bismuthinite‐argentite‐molybdenite in H 2 0‐NaCl‐CO 2 solutions from 200°C ‐300°CEcon. Geol., Vol.82
A. Afifi, W. Kelly, E. Essene (1988)
Phase relations among tellurides, sulfides, and oxides; I, Thermochemical data and calculated equilibriaEconomic Geology, 83
A. Afifi, W. Kelly, E. Essene (1988)
Phase relations among tellurides, sulfides, and oxides; Pt. II, Applications to telluride-bearing ore depositsEconomic Geology, 83
J. Riley (1974)
The tetrahedrite-freibergite series, with reference to the Mount Isa Pb-Zn-Ag orebodyMineralium Deposita, 9
D. Shenberger, H. Barnes (1989)
Solubility of gold in aqueous sulfide solutions from 150 to 350°CGeochimica et Cosmochimica Acta, 53
W. Hall, G. Czamanske (1972)
Mineralogy and Trace Element Content of the Wood River Lead-Silver Deposits, Blaine County, IdahoEconomic Geology, 67
T. Seward (1973)
Thio complexes of gold and the transport of gold in hydrothermal ore solutionsGeochimica et Cosmochimica Acta, 37
G. Gamyanin (1982)
Bismuth tellurides-Bi2Te and BiTe-in deposits of Northeast USSRInternational Geology Review, 24
Abstract The deposit under study is a hydrothermal filling‐metasomatic vein type lead‐zinc‐silver deposit, in which gold and silver can be recovered as by‐products. These metals mainly occur as microgranular native gold, electrum, stephanite, acanthite, pyraragyrite, freibergite, and native silver. Gold minerals tend to be associated with galenobismutite, native bismuth and unnamed Bi2Te. They are either enclosed in pyrite, marmatite, iron‐bearing sphalerite and galens or fill the microfissures of these minerals. Silver minerals usually occur in cleavages or fissures of galena, marmatite and pyrite, but are not associated with gold and bismuth minerals. Gold and silver mineralizations occurred later than lead and zinc, while the silver mineralization was preceded by that of gold.
Acta Geologica Sinica (English Edition) – Wiley
Published: Dec 1, 1991
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