Broken Laminae and Flaser-Like Structures

Central Southern Karavanks.

Triassic limestone displaying a horizon of disrupted and broken laminae with minimal rounding, suggesting minimal reworking and little to no transport following desiccation in subaerial or in very shallow settings.

Flaser-like interbedding (F) characterized by thin, dark micritic wisps alternating with lighter lenses of slightly coarser material reflects episodic current activity in a shallow marine setting, possibly tidally influenced.