Szukana fraza: [Abstract = The older deformations were formed during the first glaciation of the studied area ascribed to the older Elsterian stage. These structures are representing by multiple series ofimbricated thrusts that occur mainly at the open\-cast floor in the Neogene clays and coaly clays. Low\-angle to gently NNE dipping thrust planes exhibit sense of displacement towards the SSW.]

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