O jurskim i krednim sukcesijama graničnog područja Dinarske karbonatne platforme i Durmitorskog basena (granični basen Zalomka-Gacko)

Jurassic and Cretaceous successions of the Dinaric carbonate platform-Durmitor basin boundary area (Adjacent Zalomka-Gacko basin)

Abstract

The infotmation on one Dinaric Platform succession and three successions of the adjacent Zalomka-Gacko Basin in given. Summarizing data from Kunjak Potok, Lukavica and Miholjača sections it can be inferred that Zalomka unit existed as a part of the specific periplatform paleogeography until the end of the Aptian and lost its individuality in the Albian. From the Albian, covered with a transgressive sequence of basinal clastics, it was integrated with the Durmitor Basin. The Durmitor Basin progradation was succeeded and preceded by sinsedimentary tectonics when was crushed a significant portion of the platform marginal belt (documented by elements of polygenetic breccia in the basal part of a Durmitor transgressive sequence).