The general characteristics,mechanical properties,formation and evolution of the mineralization control- ling structure of Baguamiao gold deposit and its mineralization controlling characteristics are comprehensively studied.

The Baguamiao gold deposit in a sort of mesothermal hypothermal carbonate type gold deposit.

Geological features and prospecting criteria of Bacheli gold-molybdenum deposit in Heihe city,Heilongjiang province;

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.

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.

Study on the indicator element of main economic orebody in Huangbuling gold deposit,Shandong province;

Epithermal mineralization in the Western margin of the Luzon arc:Lalab gold deposit;

Geological characteristics and ore potential of No.4 ore zone in the Maquan gold deposit in Lixian county,Gansu province;