Pregled bibliografske jedinice broj: 114243
Stratigraphy of coarse grained clastics of the field Obod, Ladislavci and Crnac, Croatia
Stratigraphy of coarse grained clastics of the field Obod, Ladislavci and Crnac, Croatia // 64th EAGE conference & exhibition "Towards Integration of Geosciences", Florence 2002, Extended abstracts, vol. 2
Houten: European Association of Geoscientists & Engineers, 2002. str. P123 1-4 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Stratigraphy of coarse grained clastics of the field Obod, Ladislavci and Crnac, Croatia
Autori
Kalac, Katica ; Hernitz, Zvonimir ; Velić, Josipa ; Malvić, Tomislav
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
64th EAGE conference & exhibition "Towards Integration of Geosciences", Florence 2002, Extended abstracts, vol. 2
/ - Houten : European Association of Geoscientists & Engineers, 2002, P123 1-4
Skup
64th EAGE conference & exhibition "Towards Integration of Geosciences"
Mjesto i datum
Firenca, Italija, 27.05.2002. - 30.05.2002
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
reservoir rocks; limestone-dolomitic breccia; Upper Oligocene- Miocene; Drava depression; Pannonian basin; Croatia
Sažetak
The stratigraphyc position of the coarse grained breccias is determined as the Upper Oligocene-Miocene (Eggenburgian, Ottnangian, Karpatian and Badennian) after new analyses. Marls or sandy marls and sandstones by progressive gradation or visible sequences are located inside of a laterally to breccia. Very often, there are found kerogen siltites. For instance, it is determined that oil of the Obod field corresponds to the source rocks of the same field.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb