On the basis of geothermal gradient,geothermal current field,geothermal springs and geothermal anomalies distribution in east Qilian and take Huajialing-Wushan near SN buried deep fault as a boundary,in the east,there are geothermal field higher,more geothermal springs.So it is a mid-low temperature geothermal gield of lifted fault style,but in the west,it is just opposite to the former.The geothermal anomalies show that is subsidence basin style.All of these give an information for developing geothermal field in Lanzhou region.