Abstract
Significant quantities of silver can be accommodated in galena as a coupled substitution with Ag + Sb and/or Ag + Bi for 2 Pb atoms. The limitations of this solubility are quantified experimentally for the cubic (Fm3̅m) α-galena phase. Above 441.7 °C, the α-galena phase has complete solid solution across the Pb2S2-AgSbS2-AgBiS2 (galena-miargyrite-matildite) ternary. Dry sinter experiments at 400, 375, and 350 °C extend the known miscibility gap on the Pb2S2-AgSbS2 binary into ternary compositions. Phase equilibrium and miscibility gap data and self-consistent thermodynamic data for other high-temperature phases in this system combined with data for other sulfides and sulfosalts are used to constrain an asymmetric regular solution model for the α-galena phase (Pb2,AgSb,AgBi) S2. Phase relations in this system suggest that simple retrograde re-equilibration during cooling can produce phase assemblages and textures commonly observed in Ag-bearing ore deposits. Bulk metal ratios of deposits in conjunction with the application of this thermodynamic model may be used to understand district Ag-distribution or as an exploration tool.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
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Articles in the same Issue
- Amorphous materials: Properties, structure, and durability: Atomic structure and transport properties of MgO-Al2O3 melts: A molecular dynamics simulation study
- Amorphous Materials: Properties, structure, and durability: Oxidation state of iron in hydrous phono-tephritic melts
- Amorphous materials: Properties, structure, and durability: Quantitative Raman spectroscopy: Speciation of Na-silicate glasses and melts
- Dissolution-reprecipitation of zircon at low-temperature, high-pressure conditions (Lanzo Massif, Italy)
- High-pressure behavior of gypsum: A single-crystal X-ray study
- Presence and zoning of hydrous components in leucite from the Alban Hills volcano, Rome, Italy
- Herderite from Mogok, Myanmar, and comparison with hydroxyl-herderite from Ehrenfriedersdorf, Germany
- Application of Raman spectroscopy to quantify trace water concentrations in glasses and garnets
- Neutron diffraction study of δ-AlOOD at high pressure and its implication for symmetrization of the hydrogen bond
- A simple predictive model for the thermal expansion of AlSi3 feldspars
- New data on PGE alloy minerals from a very old collection (probably 1890s), California
- High-pressure study on lead fluorapatite
- High-pressure Al-rich hexagonal phases—What are their kin?
- Leucite at high pressure: Elastic behavior, phase stability, and petrological implications
- Thermodynamic mixing properties of Rb-K feldspars
- Demicheleite, BiSBr, a new mineral from La Fossa crater, Vulcano, Aeolian Islands, Italy
- A lattice dynamical study of the aragonite and post-aragonite phases of calcium carbonate rock
- Water in natural olivine—determined by proton-proton scattering analysis
- Factors affecting heat transfer in natural SiO2 solids
- A solution model for high-temperature PbS-AgSbS2-AgBiS2 galena
- Incorporation of molybdate anion into β-FeOOH
- Disordering of Fe2+ over octahedrally coordinated sites of tourmaline
- Raman spectroscopy of CaIrO3 postperovskite up to 30 GPa
- The thermal behavior of richterite
- The crystal structure of kelyanite, (Hg2)6(SbO6)BrCl2
- Comparison of crystallographic orientations between living (Emiliania huxleyi and Gephyrocapsa oceanica) and fossil (Watznaueria barnesiae) coccoliths using electron microscopes
- Letter. Iron partitioning between perovskite and post-perovskite: A transmission electron microscope study
- Letter. An isosymmetric phase transition of orthopyroxene found by high-temperature X-ray diffraction