
handle: 11585/545579
The Creta di Collina Formation consists of different interbedded facies. The stratotype section is composed of brachiopod-crinoidal calcarenite and calcilutite (mainly packstone, biopelsparite) with some breccias layers (rudite), brachiopod coquinite with calcilutite (packstone) intercalations, and brachiopod crinoidal calcilutite. At Porto di Cozzi the main units are dark gray calcarenite to calcilutite with scattered brachiopods and crinoid fragments (packstone), brachiopod coquinite, and brachiopod-crinoidal calcarenite (mainly packstone).
Pre-Variscan sequence, Carnic Alps, lithostratigraphy, limestone, Upper Devonian, Frasnian-Famennian, conodont biostratigraphy
Pre-Variscan sequence, Carnic Alps, lithostratigraphy, limestone, Upper Devonian, Frasnian-Famennian, conodont biostratigraphy
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