Prisotnost strukturnih deformacij enostavnega striga ni omejena samo na raziskano ozemlje, saj jih najdemo tudi na širšem prostoru slovenskih Zunanjih Dinaridov (Poljak, 1986), kjer so vezane na isti mehanizem kot na Tržaško-komenski planoti.
Presence of simple shear structural deformations is not limited to the investigated territory, they occur also in the wider area of the Slovenian Outer Dinarides (Poljak, 1986) where they are associated with the same mechanism as on the Trieste-Komen plateau.