Naslov
Mesozoic-Cenozoic Dinaric foreland basins

Autori
Lužar-Oberiter, Borna ; Gobo, Katarina ; Kukoč, Duje ; Petrinjak, Krešimir ; Aščić, Šimun ; Šamarija, Robert ; Kocjančič, Anja ; Mrinjek, Ervin ; Markotić, Lucija

Vrsta, podvrsta i kategorija rada
Poglavlja u knjigama, znanstveni

Knjiga
Sedimentary cover of the Adria and its surroundings, Field trip guidebook, 36th International Meeting of Sedimentology June 12–16, 2023, Dubrovnik, Croatia

Urednik/ci
Korbar, Tvrtko ; Kovačić, Marijan ; Vlahović, Igor

Izdavač
Croatian Geological Society (HGD)

Grad
Zagreb

Godina
2023

Raspon stranica
161-194

ISBN
978-953-6907-80-9

Ključne riječi
Vranduk Formation, Bosnian Flysch, Promina Beds

Sažetak
Synorogenic basins record the long-lasting evolution of the Dinarides mountain chain, which developed along the Adria margin, through multiple tectonic phases involving large scale ophiolite obduction and nappe stacking events. From rugged mountain landscapes in the hinterland to the clear blue waters of the Adriatic seaside, the field trip explores basin deposits ranging in age from the Jurassic to the Palaeogene, displaying a variety of sedimentary facies from deep-water pelagics, various types of gravity deposits to shallow- marine and continental environments. Visited outcrops cover the Late Jurassic-Cretaceous deep-water “Bosnian flysch", which initially formed in response to ophiolite nappe emplacement. The field trip further follows outcrops recording later phases of flexural foreland basin advancement towards the Adriatic foreland during the Cretaceous to Cenozoic orogeny. This involved major composite nappe stacking, including thick sequences of Mesozoic and Palaeogene carbonates, giving rise to the calciclastic Promina beds which record syn-tectonic sedimentation in thrust wedge-top "piggyback” basins.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

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