It is composed of quartz sandstone, shales and claystones, locally with coal interbeds.

It preserves fossils dated to the Carnian stage of the Triassic period and represents significant siliciclastic input into the European carbonate shelf due to the Carnian Pluvial Event.

Lipold as Lunzer Schichten, according to Austrian town Lunz am See.

It occurs in the Northern Calcareous Alps, Western Carpathians.

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