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EN
The paper focuses on the analysis of small-scale strike-slip faults and second-order fractures in flat-lying Cieszyn Limestones of a quarry in Leszna Górna. In the western part of the Polish segment of the Outer Carpathians, the Silesian Nappe consists of two tectonic units: Cieszyn Unit and Godula Unit. The study area is located within the Cieszyn Unit. Several different kinds of tectonic structures have been distinguished, including mesoscale strike-slip faults, en echelon arrays, tip structures and linking structures. The investigations, including geometric and genetic analysis of strike-slip faults and fractures, have enabled reconstruction of structural evolution stages. Two evolutionary models are proposed in terms of the geometries of damage zones for small displacement strike-slip fault zones.
EN
Temporal and spatial variability of mesoscale structures in the North-East Gdańsk Bay is discussed. During measurements in September 1997, variability in the upper layer was determined by convective cooling processes. Measurements made in January 1998 show that between the two periods renewal of a whole halocline water took place in the Gdańsk Bay.
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