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on the continental slope and the proximal parts of the oceanicdomain. According to the age and the microfacies(GAWLICK et al., 2016b), the limestones of the GrivskaFormation were deposited on the continental slope orin the

2) Sedimentological and microfacies studies evidenced that the Grivska Formation was deposited on the continental slope and transitional tothe Neo-Tethys Ocean. Based on the results of these investigations in the type area

the Grivska Formation occurs only as clasts and blocks in the ophiolitic mélange.Key words: Neo-Tethys continental slope, Late Triassic, stratigraphy, microfacies, ophiolitic mélange.Апстракт. Старост, микрофације и област