Basic features of the Chengbu-Taojiang basement fault along the Lianyuan basin;

The Lower Carboniferous Ceshui and Upper Permian Longtan coal series are most important in Southeast China, and can both generate and bear gas greatly in the Lianyuan coal basin, Central Hunan, China.

The Thermal History and Hydrocarbon-generating characteristics of Ceshui and Longtan Coal Series in Lianyuan,Hunan Province;

Geochemical characteristics and hydrocarbon potential of organic-rich shale in Tanzhuang Formation of Triassic,Jiyuan Basin;

Features of Paleosols from Middle Triassic Youfangzhuang Formation,Jiyuan Basin;

Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation (T_(2-3)), Jiyuan Basin, Henan Province;

Mineralogy evidence of shoshonite rock series from Shengyuan basin and it s adjacent area;

Using the modern structural analysis on the characteristics of basement lithologics and lithofacies, basement structures and its evolution regularities the author suggests that the metamorphic deformed basement of Shengyuan basin creats extremely favourable geologic background for the ore formation of uranium and polymetal.

Based on the isotopic dating data of volcanics and recent research achievements of age boundary between Jurassic and Cretaceous systems, it is suggested that the volcanic series in Shengyuan basin must be attributed to Lower Cretaceous.