The Dzhaur tungsten-polymetallic deposit is located in the northern Sikhote-Alin in the upper reaches of the Dzhaur River, a left tributary of the Khungari River. Its study is of particular interest because it is the first skarn-type deposit in the northern Sikhote-Alin. Besides, the Dzhaurskoe deposit belongs to the category of few, but very important for understanding the genesis of skarn deposits of skarn type, deprived of connection with limestones.