Skoči na glavni sadržaj

Geoadria, Vol. 20 No. 2, 2015.

Pregledni rad

https://doi.org/10.15291/geoadria.2

Definition of new Pliocene, Pleistocene and Holocene lithostratigraphic units in the Croatian part of the Adriatic Sea (shallow offshore)

Tomislav Malvić orcid id orcid.org/0000-0003-2072-9539 ; Sveučilište u Zagrebu, Rudarsko-geološko-naftni fakultet, Zavod za geologiju i geološko inženjerstvo, INA-Industrija nafte d.d., Sektor za geologiju i inženjering
Josipa Velić ; Sveučilište u Zagrebu, Rudarsko-geološko-naftni fakultet, Zavod za geologiju i geološko inženjerstvo
Marko Cvetković orcid id orcid.org/0000-0002-4555-6083 ; Sveučilište u Zagrebu, Rudarsko-geološko-naftni fakultet, Zavod za geologiju i geološko inženjerstvo
Marko Vekić ; Sveučilište u Zagrebu, Rudarsko-geološko-naftni fakultet, student diplomskog smjera
Marijan Šapina ; Sveučilište u Zagrebu, Rudarsko-geološko-naftni fakultet, student diplomskog smjera

Puni tekst: hrvatski pdf 8.168 Kb

str. 85-108

preuzimanja: 1.136

citiraj

Puni tekst: engleski pdf 8.168 Kb

str. 85-108

preuzimanja: 536

citiraj

Sažetak

Exploration of Pliocene, Pleistocene and Holocene deposits in of the Croatian Northern Adriatic and Southern Dalmatia (coastline) offshore is presented in this paper. It was a way to describe the existing lithostratigraphic units in Croatian Po River sediments and to determine such units in the depositional area of Neretva River. Both systems have been influenced by sea-level fluctuations during the Quaternary, resulting in significantly decreased sea depths and increased subaerial exposure during glacial periods, especially in the Northern Adriatic. In the Croatian part of Po Depression, two new formations were mentioned – Istria (Pliocene) and Ivana (Pleistocene, Holocene). Three new lithostratigraphic members were described within Ivana Formation, namely Anamarija, Katarina and Izabela. Further south, in the Southern Dalmatia shallow offshore, Pliocene, Pleistocene and Holocene deposits were named the new Neretva Channel Formation. This formation was further divided into Neretva Sands (sometimes equivalent for entire formation) and the (Quaternary) Mali Ston Bay Member. No typical Pliocene lithotype has yet been recognised.

Ključne riječi

lithostratigraphy; Pliocene; Pleistocene; Holocene; Adriatic; Croatia

Hrčak ID:

151719

URI

https://hrcak.srce.hr/151719

Datum izdavanja:

30.12.2015.

Podaci na drugim jezicima: hrvatski

Posjeta: 3.341 *