As one of several larger deposits in Tibet, Jiama deposit went through submarine sedimentary exhalation in the late Yanshanian period and porphyry mineralization in the Himalayan period, by which the stratiform orebodies and porphyry ones were formed respectively.

The diagenesis and lapidofacies of Yanchang formation Chang3 reservoirs in Baibao Area;

Quantitative characterization of diagenesis and prediction of favorable areas in the west slope of Yuanyanggou subsag;

Effect of abnormal high pressure on diagenesis and pore evolution of Mesozoic reservoirs in Kuga depression;

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

Initial discussion on geological characteristics of the Erbahuo silver deposit of Wengniute Inner Mongolia and its mineralization;

Hydrothermal mineralization of Au (Ag)-polymetallic ore deposit in the volcanic rock series of the Xiong'er Group;

Geological characteristics and metallogenesis of Sawayaerdun gold deposit in southwest Tianshan Mountains, Xinjiang;

The possible connection of the earth electric force and magnetic force controlling metallogenesis;

Post-orogenic dike complexes and implications for metallogenesis;