Paleogene adamellite and feldspar granite developed in Tengchong-Lianghe area, Western Yunnan, recorded magmatism information in the collision between Indian and Asian continents. The LA-ICP-MS zircon U-Pb age of typical adamellite is 51.4±0.4Ma, and Hf modal ages are 1.46-1.55Ga, εHf(t) values are -6.65 to -5.30. Major elements of Paleogene granite from Tengchong-Lianghe area, are characterized by high SiO2 (68.96%-78.68%), K2O (4.56%-6.29%) and Al2O3(12.40%-16.42%), and have K2O/Na2O ratios of 0.93-7.24, A/CNK values of 0.99 to 2.31 with Al2O3>(K2O+Na2O)，belong to metaluminous-strongly peraluminous high K calc-alkaline granite; Their trace elements show strong negative Eu anomalies with Eu/Eu*values of 0.19 to 0.51, enrichment of Cs, Rb, Pb but depletion of Sr、P、Ti、Ba、Nb、Ta. Elements geochemical features signified that these granites might be generatedfrom upper crust by partial melting of metagraywacke. Based on the regional geology, we suggested Tengliang granites (62-51Ma) magmatic response events on the peak period of India-Asia collision.