On the south of the Russian Far East, a new promising type of mineral resources has been identified-metal-bearing titanium-bearing intrusions of ultrabasic rocks of the Sikhote-Alin orogenic belt. The main features of the mineralogy and geochemistry of gold-ilmenite and gold-antimonite ores that spatially and genetically related to one of these intrusions - Ariadnenskaya, are determined. The isotopic composition of sulfur in sulfides of manifestations of titanium and antimony mineralization indicates a common source of ore matter. An in-depth study of these metal-bearing formations will expand the prospects for the raw material base of strategic metals in Primorsky Krai.

Topics
Geochemistry, Mineralization, Mineralogy, Transition metals
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