Naslov
Neogene deposits of the western slopes of the Psunj Mt., Croatia: an overview of historical background and actualisation of geological research

Autori
Vrsaljko, Davor ; Bošnjak, Marija ; Jarić, Anja ; Sremac, Jasenka ; Malvić, Tomislav

Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni

Izvornik
Mathematical methods and terminology in geology 2020 / Malvić, Tomislav ; Barudžija, Uroš ; Bošnjak, Marija ; Sremac, Jasenka ; Velić, Josipa - Zagreb : Rudarsko-geološko-naftni fakultet Sveučilišta u Zagrebu ; Hrvatsko geološko društvo, 2020, 63-76

ISBN
978-953-6923-42-7

Skup
3rd Croatian scientific congress about geomathematics and terminology in geology: Mathematical methods and terminology in geology 2020

Mjesto i datum
Zagreb, Hrvatska, 10.10.2020

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Neogene ; stratigraphy ; petroleum geology ; Psunj Mt. ; Croatia

Sažetak
On the crystalline rocks of the western slopes of the Psunj Mt. disconformably lie Neogene sediments with recorded deposits from the Lower Miocene to the Quaternary period. The basal Neogene sediments are in the older papers defined as “Oligomiocene” or “preTortonian”, today corresponding to the Lower Miocene sediments. These freshwater and marine-brackish sediments are transgressively overlain by the marine middle Miocene sediments. Badenian deposits are distributed as a continuous belt along the western slopes of the Psunj Mt., east from Pakrac and Lipik, with various lithofacies diversity. In the wider area they are a part of the structure Bijela Stijena–Novska. Lower Sarmatian rhythmic sediments conformably lie on the Badenian sedimentary rocks. The brackish and freshwater development is marked by the continuation of the Upper Miocene sedimentation, and Pliocene sediments with complete “Paludina beds” development mark the end of the Neogene. Dominant is the anticlinal structure – structure nose with an axis Bijela Stijena– Novska. In the core of the structure are crystallinic rocks. Neogene sediments are periclinal and almost continued along the limbs and forehead of the structure.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

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