Abstract:In recent years, one derivative processing method is Thete Map method. By using maximum to delineate magnetic geological boundaries. The main steps of its algorithm are to calculate the ratio of vertical first derivative and total horizontal derivative. By analyzing the thete maps in different magnetic models, correspondence law of thete map and the boundaries of upright magnetic bodies, tilt magnetic bodies, rock and skarn have been summarized. This method have references to delineate fault structure and geological boundary by using gravity method.