engleski

Subtidal-supratidal cycles in the Late Permian of the Velebit Mt. (Croatia)

Evidences of cyclic sea-level changes can be traced within the Late Permian carbonate sequence in the central part of the Velebit Mt.(SW Croatia). Subtidal, intertidal and supratidal facies can be recognized through microfossil communities and sedimentary structures. Regressive episodes are more frequent in the uppermost part of the sequence.

Carbonate platform; Subtidal-supratidal cycles; Late Permian Velebit Mt.; SW Croatia.

nije evidentirano