Ottnangian lacustrine sedimentation on Mt. Medvednica: facies, depositional environments, and tectonic controls (Pannonian Basin System, Croatia) (CROSBI ID 472943)
Prilog sa skupa u zborniku | izvorni znanstveni rad | domaća recenzija
Podaci o odgovornosti
Pavelić, Davor ; Avanić, Radovan ; Zupanič, Jožica
engleski
Ottnangian lacustrine sedimentation on Mt. Medvednica: facies, depositional environments, and tectonic controls (Pannonian Basin System, Croatia)
The evolution of the Ottnangian lake was related to synsedimentary tectonics. The first phase consists of the fine-grained swamp deposits, overlain by carbonate deposits of the lake margin, and marls and thin turbidites of a deeper lake realms. These sediments reflect continued tectonic subsidence and deepening. The second phase shows a coarsening-upward trend with an increase of the proportion of clastic deposits, reflects delta progradation, and may be interpreted as a consequence of a relative tectonic quiescence. The third phase includes very silty marls and turbidites, and indicates renewed tectonic activity and deepening. Marine transgression in Karpatian, which terminated the evolution of the lake, is explained by the opening of the connection with Mediterranean sea due to tectonic subsidence.
lacustrine sedimentation; tectonic contol; Early Miocene (Ottnangian); Mt. Medvednica; Pannonian Basin System; Croatia
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Podaci o prilogu
339-343.
2000.
objavljeno
Podaci o matičnoj publikaciji
2. hrvatski geološki kongres : Zbornik radova = Second Croatian Geological Congress : Proceedings
Vlahović, Igor ; Biondić, Ranko
Zagreb: Hrvatski geološki institut
953-96520-7-3
Podaci o skupu
Hrvatski geološki kongres (2 : 2000)
poster
17.05.2000-20.05.2000
Cavtat, Hrvatska