Granites and Earth Evolution.
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PHYSICO-CHEMICAL MODELING OF GOLD-BEARING SULFOARSENIDE SOLUTIONS IN THE GRANITE SYSTEMS

Vilor N.V.*, Kazmin L.A.**

*Institute of Geochemistry SB RAS, Irkutsk, Russia, vilor@igc.irk.ru,

**Research Center of Geotechnology FED RAS, Petropavlovsk-Kamchatsky, Russia, kazmin@igc.irk.ru


Sulfoarsenide systems form in granite pluton upper intrusive areas. Its redistribute gold, concluded in early mineral associations, and concentrate the metal inside of arsenopyrite ore type. Physico-chemical modeling on the “Selector” program complex basis is used for the determination of arsenic important geochemical role for the high production gold ore formation, which connected with granite massifs. This calculation method has some difficulties, which are deficit of the chemical (compound composition) and thermodynamic (thermodynamic constants) information.

The thermodynamic base creation (gt function calculation is the first of all) for Fe - As – Na – S – Cl – H –O system components includes its coordinate procedures for 3 additional systems: 1) solution + magnetite, 2) solution + pyrite and 3) solution + arsenopyrite (+lollingite). General system includes the equilibrium of Fe oxides, sulfides and arsenides with wide pH interval of chloride solution. Modeling was consisted of the coordination of these 3 systems.

The calculated system composition is, mol: arsenopyrite 1, H2S 0.66 ÷ 0.92 x 10-3, HCl and NaOH 1 x 10-6 ÷ 0.001, H2O 1 kg. Calculated parameters are t oC 100-300, P - from the saturation water vapor pressure to 300-500 bars. The number of solution particles is 515, gases 105, solid minerals 47.

Arsenic is in the solution as thioarsenic acid H3AsS30 (less that 2x10-2 m) with presence As(OH)2HS0 and As(OH)(HS)+ complexes in the acidity interval from 3.53 to 6.36 and H2S concentration from 0.69 x10-3 to 0.92 x10-3 m. Asenite acid H3AsO3 dominates about 300 0C under the saturation water vapor pressure. Fe transports as the hydrosulfide group composition: Fe(HS)+, Fe(HS)2 0, Fe(HS)3- and concentration equal from 5.4x10-4 to 1.9 x10-2 m. The supposed ferrothioarsenites Fe(1-2)H(0-3)As(1-4)S(1-7)(-1÷+4)are minor for hydrothermal process used conditions.