Search for: [Abstract = "At the locations showing strong lithological variability the deformations are mainly discontinuous, like thrusts and glaciotectonic slices. To the contrary, within the monotonous fluvioglacial sediments, the fold defarmation accompanied by the normal faults are observed. The results of the mesostructural measurements indicated the glaciotectonic transport in ESE direction resulting from the strike of the Sudetic Block border."]

Number of results: 1