The comparision of mineralisation volcanogenic deposits of gold-sulfide formation wfs pursued. The deposits Lebedinoe (Central Aldan), Radka, Chelopech, Elshica (Boulgaria) were formed atthe similar of geological conditions. These deposits investigated in the different degree, but they have the similar mineral-geocamical peculiarities. The rare-metals minerals are typical for Radka deposit. The tellurium minerals are typical for Elshica deposit. Mineralisation of Chelopech and Lebedinoe deposits are binding member between mineralisation of Radka and Elshica deposits. The supposition was made that the rare-metals mineralisation will be discovered at the ores on the more deep horisonts of Elshica deposit. It is possible that diverssified rare-metals (Ge, Ga, In) mineralisation will be discovered at the ores Lebedinoe deposit during the further investigations.
Keywords: rare-metals mineralisaton, tellurium minerals, fahlore, deposits Lebedinoe, Chelopech, Radka, Elshica.