Аннотация:The differentiated Bushveld complex is studied by remote-space and gravimagnetic methods. The
syncline of Western Bushveld is recognized in the southwestern part of the complex, which is characterized
by a radial and ring structure of the higher order. The structures, which control the localization of Pt mineralization,
are revealed and the possible use of the Landsat 7 ETM+ multizonal space survey is shown for recognizing
the rocks of the Basal, Critical, Main, and Upper zones of the norite complex of Western Bushveld.