Finally it is discussed the strategic value and significance of the water transfer to central Yunnan province project to the social economic development in Kunming and the ecological reconstruction of Dianchi watershed.

,as well as three other indeterminable species are for the first time found in the Lannijing and Jishanpo sec-tions of the Late Jurassic Tuodian Formation in central Yunnan Province,Southwest China,in2002.

The metallogenic belt in Central Yunnan Province shows multi-scale geological anomaly controlled by multi-grade structural system.

Establish Forecast Model of Central Yunnan Heavy Rain-Rainstorm Winth Weather System of Low Pressure Vortex;

Mesoproterozoic Soft-sediment Deformational Structures in Central Yunnan, China and Their Geological Implications;

The geological historical background of redbed in Central Yunnan and the distribution range of redbed are introduced in this paper,with the main focuses on the lithological character of principal strata and the geological structure in this area.

The Central Yunnan Basin is a Mesozoic,Cenozoic basin was formed in the long-term uplifted Sichuan-Yunnan old continental nucleus(customary Kangdian old land) after acutely subsided during Late Indo-Chinese Epoch.