Abstract: The Haliheng gold deposit is located in the Eastern Junggar Variscan fold belt, belonging to the eastern section of the Ertix gold belt, with developed fault structures. There are three soil assemblage anomalies in the area, among which gold deposit has been found in No. 2 anomaly and proved as ductile shear zone type. The No. 3 anomaly covers a large area, with high Au anomaly value, well zonation and obvious concentration center. The geological characteristics of the anomalies resemble those of the known orebodies, with a good prospecting potential.