Naziv vsebine
Small Scale Thrusts
Site
Central Southern Karavanks.
Notes
Micro-thrusts (arrows) within the laminated Triassic limestone suggest localized compression during soft-sediment deformation, potentially linked to slumping.
Further observations
The layer thickening in areas indicated by T is more likely due to compression and buckling rather than thrusting, as there is no clear evidence of displacement or shearing. The faults are likely a later brittle event.
