DYNAMIKA WÓD PODZIEMNYCH W STREFACH FLEKSUROWO-USKOKOWYCH NA PRZYKŁADZIE REJONU OŻAROWA (WYŻYNA KIELECKA)

Marcin Kos

Abstract


DYNAMICS OF GROUNDWATER IN THE FAULT-FLEXURAL ZONES ON THE EXAMPLE OF THE OŻARÓW REGION (KIELCE HIGHLAND)

Abstract. Fault-flexural zones are numerous in the northeastern part of the Holy Cross Mountains Mesozoic margin, and the Lublin Trough. Dynamics of groundwater in these zones is conditioned by tectonics, mainly by transversal faults. This was presented on the example of the Sienno-Ożarów flexure (Kielce Highland). Results of investigations and an analysis of archival dates allowed to proof an existence of the hydraulic connection between Jurassic and Cretaceous aquifers. An evidence of the hydraulic connection between these aquifers allowed to show the continuous groundwater flow between the Jurassic and Cretaceous aquifers.


Keywords


kontakt hydrauliczny, strefa drenażu, dział wód podziemnych, dynamika wód podziemnych, strefy fleksurowo-uskokowe, Wyżyna Kielecka.

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