Występowanie łupliwości we fliszu wschodniego Podhala

Abstract

OCCURRENCE OF CLEAVAGE IN THE FLYSCH DEPOSITS OF THE EAST PODHALE REGION

The study embraces the western part of the East Podhale region (Fig. 1), where a series of measurements of cleavage planes were made. Since the fracture planes are, as a rule, perpendicular to bedding planes, the measurements were restricted only to a determination of strike azimuth.

When studied, a dependence of course, form and density of fracture planes upon the thicknesses of banks and upon their lithological development was established and a system of mineralized crevices (mineralization by white or gray calcite) was distinguished.