The Binchuan region is located in a seismically active area in northwestern Yunnan,China.The detailed crustal structure is important to understand the tectonic evolution and to assess the seismic hazard in the study area.With a 2-D dense array deployed in this region,we use teleseismic receiver function traditional imaging methods,including the H-κ and common-conversion-point stacking methods,to derive high-resolution crustal thickness and vp/vs ratio maps.Our results indicate that the crustal thickness increases from ~40 km to ~46 km in the south-north direction,and the average crustal thickness beneath the Binchuan basin is ~42 km.Our results agree with previous results but have higher resolution due to dense interstation spacing.