Szukana fraza: [Abstract = Complicated deformations are visible mainly in sandygravel sediments and muds between two till horizons, however the tills are also locally deformed. The following deformational structures were distinguished\: diapirs, loadings, complementary shears, different fold types, slices, detachments, duplexes, cylindrical shears, normai and reverse faults. Ifs very difficult to state which of the structures have glaciotectonic origin, which one reflect basement tectonics and which of them have neotectonic origin.]

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