Zaradi horizontalnih premikov vzdolž dinarsko usmerjenih prelomov so nastale t.i. strukture preprostega striga in ešalonirane metrske, dekametrske in večje gube v smeri severovzhod - jugozahod.
Owing to horizontal displacements along the dinaric trending faults the so-called simple shear structures were formed, as well as the echelon-like arrangement of metric, dekametric and larger folds of northeast-southwest striking.