The system of discontinuous dislocations of the Solotvyno deposit and the methodology of their study on the example of one exposure

Abstract

The purpose of this work was a detailed study of discontinuous dislocations of different levels (from tectonic cracks to discontinuous faults) on one of the rock outcrops near the area of the Solotvyno salt deposit. The research area tectonically refers to the Solotvyno depression of the Transcarpathian depression and consists of tuffaceous and sandy-clay rocks of early Neogene age. It was established that the "Solotvyno" site has a complex of geological and tectonic structures with the development of folded and discontinuous dislocations.