The Buerkesidai gold deposit is located in the eastern Sawuershan, the north-western margin of the Zhunge'er Basin, Xinjiang, and is one of the most typical supergene-structural altered-rock type gold deposits in the Zhunge'er area.

The Buerkesidai gold deposit occurs within lower Carboniferous carbon-bearing rocks.

Base on the study of geological features and factors of controlling mineralization of Kuoerzhenkuola gold deposit and Buerkesidai gold deposit, the authors consider the two deposits have the same or similar geological characters, the orebody is existed in the same time rocks, mineralization is controlled by both the same old volcanic apparatus and regional fault.

~(40)Ar-~(39)Ar Isotope Chronology of the Buerkesidai Gold Deposit, Xinjiang;

This paper has studied detailly the tectono-metallogeny of the Buerkesidai gold ore deposit, and has proposed a tectono-metallogenic model for the Buerkesidai gold ore deposit:primary gold-bearing source bed→gold-bearing source bed→tectonoclastic-alteration rock belt.

The study on typomorphic peculiarities such as chemical composition, fluid inclusions, stable isotope and time space evolution of pytite, quartz and arsenopyrite from Shaerbulake gold deposit in Xinjiang suggests that the mineralization mechanism of the deposit is percolating of thermal mine in the rocks.

The main fault plane of the fractural zone in Sarbulak gold deposit is not so continuously that it pinches out and reappears laterally and is characterized mainly by brittle then ductile and strike-slip deformation.