engleski

Evolution of Depositional Environments from the Palaeozoic to the Quaternary in the Karst Dinarides and the Pannonian Basin

The book comprising more than twenty papares, with the contributions of almost forty collegues of different generations and specialities, represents a summary of today, s understanding of the geology of the region, which is mostly composed of sedimentary rocks, both siliciclastic and carbonates.The book have 6 parts: Evolution of the Istrian part of the Adriatic Carbonate Platform from the Middle Jurassic to the Santonian and Formatin of the Flysch Basin during the Eocene ; Mein Events Recorded in the Sedimentary Succession of the Adriatic Carbonate Platform from the Oxfordian to the Upper Santonian in Istria ; Eocene Carbonates and Flysch of the Pazin Basin ; The Jurasic Succession of Mt. Svilaja ; Lower Cretaceous Platform Deposits of the Mt. Svilaja ; Regionally Important Lower Cretaceous Lithofacies Units in the Mt. Biokovo ; Platform Dynamics During the Late Cretaceous and Early palaeogene - Exernal Dinarides, Dalmatia ; Break-Up of Pangea: Evidence from Permo-Triassic Sedimentology and Ore-Deposits (W Slovenia and W Croatia) ; Val gardena Formation (Permian: Uranium Mine Žirovski Vrh (W. Slovenia) ; Formation of the Middle TriasicHg-SEDEX deposit - Mercury Mine Idria ; Carbonate Platform Environmet from the Middle to Late Permian of the Central Velebit ; Permian and Lower Triassic Facies of the Velebit Mt. and Gorski Kotar ; An Outline of the Evolution of the Croatioan Part of the Panonian Basin System ; Regional Subaerial Unconformities in Shallow-Marine Carbonate Sequence of Istria.

Depositional environments; Adriatic Carbonate Platform; Karst Dinarides; Panonian Basin; Paleozoic; Jurassic; Kretaceous; Tertiary; Croatia

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