Studing the tectogenesis in the middle course basin of river latorytsia based on analysis of basic releif surfaces
A possibility of studying the tectonic processes in the folded mountain areas using the structural morphometry and the GIS-analysis has been demonstrated. The results of analysis of basic surfaces, constructed based on non-uniformly scaled topographic maps, have been discussed. The correlations have been revealed between the orography forms, tectonic and volcanic structures on the Carpathian model polygon.