Behavior of Au, Sb, Te, As, and Bi in heterophase chloride oxidized fluids at 700°C in the pressure range of 109–124 MPa: Evidence from the study of synthetic inclusions

The heterophase state of magmagene fluids has been established for many hydrothermal deposits related to the development of oremagmatic systems of various geochemical profiles. The processes of heterogenization are most clearly reflected on the porphyry CuMoAu, SnW, some CuNiPt, Au skarn (AuCuTe typ...

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Veröffentlicht in:	Doklady earth sciences 2011-03, Vol.437 (1), p.349-351
Hauptverfasser:	Borovikov, A. A., Bul’bak, T. A., Borisenko, A. S., Palesskii, S. V.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth and Environmental Science Earth science Earth Sciences Gases Geochemistry Mineralization Oxidation
Online-Zugang:	Volltext
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