Morfostrukturní a geofyzikální analýza vybraného území v rámci GNSS sítě Morava

Abstract

The presented thesis deals with morphostructural analysis and analysis of geophysical data within a defined territory of north Drahany Highlands. This is an area of increased seismotectonic activity at the crossing of Nectava-Konice fault system with Boskovice Furrow marginal faults. The area is part of the Geodynamic Network MORAVA, where measurement of movement tendencies is carried out using GNSS technology. During the study morpholineament and structural analysis have been used to distinguish main deformation phases during tectonic evolution of the area and to identify linear structure manifestation of geological structure in the relief. In the second part magnetic and gravity anomal fields have been analysed within the area. The outputs of all the analyzes have been compared and discussed. The main results of the thesis are findings concerning geological structure manifestation and character of structural predisposition of geomorphological forms in the area.