Zhahe gold deposit is located in the middle-to-south part of the Sawuer Late Paleozoic island arc of the Junggar Plate. Orebodies occurring in diorite invaded the late Hercy-early Indosinian and the surrounding area of diorite. Two groups of faults, i.e.  the north-west and north-east faults, exist in the mining area. The north-west faults have been the migration channels of metallogenic hydrotherm and the ore-forming place for the concentration of gold elements. Magma provided the gold metallogenic material and part of hydrotherm. Zhahe gold deposit belongs to the structural alerted-rock type. And a mineralization analysis showed that it is a medium-low temperature hydrothermal deposit.