Występowanie łupliwości we fliszu wschodniego Podhala

Authors

  • Jędrzej Pokorski

Abstract

OCCURRENCE OF CLEAVAGE IN THE FLYSCH DEPOSITS OF THE EAST PODHALE REGIONThe 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.

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Issue

Vol. 9 No. 3 (1965)

Section

Articles

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