Carbonate Platform Environment from the Middle to Late Permian: Paleozoic Sediments of the Central Velebit Mt. (Croatia) (CROSBI ID 503516)
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Podaci o odgovornosti
Sremac, Jasenka ; Marjanac, Tihomir
engleski
Carbonate Platform Environment from the Middle to Late Permian: Paleozoic Sediments of the Central Velebit Mt. (Croatia)
The Upper Palaeozoic tectonic belt of the Mt. Velebit and Lika region represents the best known and most completely developed Palaeozoic area in Croatia. Sediments here range from the Pennsylvanian (Moscovian) to the Late Permian in age. Carbonate sediementation took part sporadically during the Carboniferous and Early Permian. Intensive tectonic uplift at the beginning of the Middle Permian caused the formation of prominent relief and its rapid erosion, followed by sedimentation of terrigenous molasse sediments. After the phase of instability, lowering of the relief enabled the stabilization of the area and formation of carbonate platform environment that existed until the end of Permian. Rapid production of carbonate material resulted in more than 900 m of carbonate sediments, dolomites and limestones, rich in diverse and numerous fossils from Middle to Late Permian age.
carbonate platform; reefs; Permian; Velebit; Dinarides
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Podaci o prilogu
147-150-x.
2003.
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objavljeno
Podaci o matičnoj publikaciji
Field trip guidebook : evolution of depositional environments from the palaeozoic to the quaternary in the Karst Dinarides and the Pannonian Basin / 22nd IAS Meeting of Sedimentology
Vlahović Igor ; Tišljar, Josip
Zagreb: Hrvatski geološki institut
Podaci o skupu
22nd IAS Meeting of sedimentology,
predavanje
17.09.2003-19.09.2003
Opatija, Hrvatska