On Cheng Shilian and His Xiaoyasiji;

Self-consciousness of Scholar-Bureaucrat in Political Resentment Poems of Xiaoya;

On the Etiquette and Music Cultural Decline from West Zhou to Chunqiu through xiaoya of The Book of Songs;

The juxtaposition of Guofeng and Xiaoya and its meanings in literary interpretation;

Eco-environment change and influence factors in the Songnen plain since the Quaternary;

Discovery of Quaternary potassic volcanic rocks and the establishment of Sailipu Formation in West Gangdis of Tibet, China;

Character of heavy minerals in Quaternary sediments in Yichang area and its relationship with cut-through of the Yangtze Three Gorges,China;

The exploration method of late Quaternary shallow biogenic gas reservoirs in Hangzhou Bay area.;

Environmental Changes of Late Quaternary in Source Rigion of The Huanghe River;

Evolution of Paleovegetation and Paleoenvironment of Late Quaternary on Basis of Spore-pollen Analysis in Shanghai Region;

Quarternary sediments in Shenyang are widely distributed with NE thin and SW thick,which basically is multilayered sand compound texture:the surface is a relatively thin clay,downward relatively thick and grading layers of fine medium grained sand,coarse grained sand,gravelly sand,and gravel.

In the Tathang and Yan Mountains,incised and meandering valleys formed in Quarternary.