Minerals of bismuth and antimony in original deposits of zarmitan gold zone, located in granitoid intrusion (Uzbekistan)

Modern methods of nanomineralogy (electron microscopy, electron probe microanalysis) were used to study the ores one largest industrial facilities Uzbekistan - Zarmitan gold zone, which includes Zarmitan, Urtalik, Guzhumsay deposits, are located in Koshrabadgranosyenite massif. The development / Au-W Au-Bi-Te Au-As Au-Ag-Te Au-Ag-Se Au-Sb-Ag Au-Hg types ores. Productive mineral-geochemical gold-bismuth-telluride, represented by maldonite, tellurides, and sulfosalts bismuth: hedleyite, joseite, tsumite, tetradymite, matildite, treasure, also gold-silver-sulfoantimonide type aurostibite, sulfoantimonidesPb, Fe, Ag: plagionite, jamsonite, boulangerite, goodmundite, ovichiite gold-pyrite-arsenopyrite with nanogold, lellingite, gersdorfite. main resource is provided Au-Bi-Te, Au-Sb-Ag, partially types. objects zone belong orogenic deposits associated intrusion. established mineral geochemical features direct signs prospecting, typification, assessment hidden mineralization belts.