The work shows the results of measurements magnetization (natural complete, natural residual and induced magnetization, inclination of angles complete and residual magnetization, ratio Koenigsberger) titanomagnetite ores Gusevogorskoye deposit in natural situ. The data was received by results of a three-component borehole magnetometer, measurement in explosive holes in Kachkanar. It is concluded that the observed changes in the natural residual magnetization indicate the formation of titanomagnetite ores in different thermodynamic areas as a result of subsequent geological processes that led to the disintegration of solid solutions. The main magnetic phase of these deposits were quite similar in composition and magnetic structure.
