The Konder massif represents a pipe-like mantle body that intruded the Archean crystalled basement of Aldan Shield. The rounded dunite body of 5.5 km in diameter is bordered with a pyroxenite zone about 150-200 m in width. This dome-like structure was probably formed because of diapiric intrusion of solid and hot dunite-pyroxenite body. Magnetic susceptibility x values of dunite for three radial profiles depend on distance and have multiextreme character (the contact dunite-pyroxenite is accepted as zero point). The first from the pyroxenite ring maximum reaches the greatest value (~ 0.01 unit SI). Further, with increase of distance from periphery of the dunite massif, amplitudes of extremes naturally decrease. The distance between extremes is 150-200 m. In this case local shift bands arise on the interface of a deformed dunite-pyroxenite body and are distributed into all its volume, representing damper zones, which interfere destruction of the body. We observed thin structure of conjugate deformation bands in zones of minimum values of %■ Distance between these bands are ~1 m. These bands are “massive” weather-proof dunite in opposite to schistose one. The “massive” dunites” characterize high coercive force Hc and density of defects p (plastically deformed zones), because Hc ~ yfp Thus, variations of magnetic properties of rock are an indicator of localization of plastic deformation at different hierarchy levels.