Naziv vsebine
Current Lineation
Site
Central Southern Karavanks.
Notes
The faint, parallel linear structures developed along laminae—interpreted as current lineation—suggest deposition under fast, unidirectional currents, likely within a shallow marine shelf or ramp setting influenced by storm-generated flows. ?Permian.
Further observations
The lineation is actually exposed on natural parting planes, where detachment occurred along weaker bedding-parallel laminae within mudrock/fine sandstone.
