Spękania ciosowe w skałach detrytycznych sarmatu południowego obrzeżenia Gór Świętokrzyskich
Abstract
Omówiono zespoły spękań o charakterze ciosowym, występujące w zwięzłych skałach detrytycznych sarmatu na południowym obrzeżeniu Gór Świętokrzyskich. Wyjaśniono ich genezę i związki z budową tektoniczną podłoża paleozoiczno-mezozoicznego.JOINT IN DETRITAL SARMATlAN ROCKS AT SOUTHERN MARGIN OF THE GÓRY ŚWIĘTOKRZYSKIE MTSThe sets of·strictly oriented joints and open joints were observed in detritical hard rocks of Sarmatian age at southern border of the Góry Świętokrzyskie Mts. The author interpreted them as the tension and shear joints. The joints represent an effect of post-Sarmatian vertical tectonic movements, which have renewed old dislocations of sub-Miocene basement and several zones of joints and depressions in the top of Lithothamnium Limestone and Gypsiferous horizonts of Badenian age. These movements had also influenced on the formation of Recent river system on the investigated area.Downloads
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