engleski

Coastal Dinaric Flysch Belt: Paleotransport model for the Pazin Basin and the role of a foreland uplift.

Sedimentary infill of the Pazin Basin, Istria, shows that the Eocene foreland basin in coastal Dinarides received the detritus from the outer (Adriatic) side, and not only from the SW indicates the existence of a carbonate area, which was partly exposed and partly covered by shallow sea characterized by carbonate deposition. This high area embraced the southern part of the present-day Istrian peninsula, and continued into the Adriatic offshore. This foreland uplift was undergoing deformation during the evolution of the Pazin Basin.

paleotransport; foreland basin; foreland uplift; flysch; Eocene; Pazin Basin; Dinarides; Croatia

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