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 the few, but very important for understanding the genesis of skarn deposits of skarn type, lacking connection with limestones.