Magnetic susceptibility of sediments in the northern edge of the Dniepr-Donetsk depression was analyzed. Possibilities of c-metering implementation for vertical division and investigations of geological cross-section, also as correlations of defined elements were shown.
Aim. Sediments of Solohiv suite (upper Visean) were investigated to show capebilities of -metering in adjustment of facial boundaries. This sediments correlates with productive horizons (PH) B-23, B-22, B-21 and productive layers from micro-fauna (MF) horizon XIIa in Dnipro-Donetsk Depression. Investigated Chervonozavodske and Lucenkivske deposits have commons features in structure and lithographic of PH.