Rozpoznanie pokryw lessowych metodą pseudotomografii oporu

Abstract

A main aim of research work was to recognize loess covers by geoelectrical method for three tipped areas, to define loess thickness and show their variability. Resistivity imaging method was used. To research chose Kańczuga Plateau, Nałęczów Plateau and Prydniestrov’ja region (Ukraine). There were used resistivity imaging methods, and the work results were corelated with geological documentation of the research area. The research showed variability in loess covers related to their stratigraphy and allow determine thickness loesses deposit.