Pregled bibliografske jedinice broj: 750136
Eocene/Oligocene Boundary (Vascus Member) in the Western part of the Tripolitania Basin, Libya
Eocene/Oligocene Boundary (Vascus Member) in the Western part of the Tripolitania Basin, Libya // Tertiary to recent larger Foraminifera. Their depositional Environments and Importance as Petroleum Reservoirs / Thompson, Peter R (ur.).
London : Delhi: London : Kingston University, 1998. str. 12-12 (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Eocene/Oligocene Boundary (Vascus Member) in the Western part of the Tripolitania Basin, Libya
Autori
Premec-Fuček, Vlasta ; Hernitz Kučenjak, Morana ; Mesić, Ivan, A.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Tertiary to recent larger Foraminifera. Their depositional Environments and Importance as Petroleum Reservoirs
/ Thompson, Peter R - London : Delhi : London : Kingston University, 1998, 12-12
Skup
Conference - Workshop - Field Trip Tertiary to recent larger Foraminifera. Their depositional Environments and Importance as Petroleum Reservoirs
Mjesto i datum
London, Ujedinjeno Kraljevstvo, 15.02.1998. - 19.02.1998
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
eocene/Oligocene boundary; foraminfera; Libya
(Conference - Workshop - Field Trip Tertiary to recent larger Foraminifera. Their depositional Environments and Importance as Petroleum Reservoirs)
Sažetak
Exploration well in the western part of the Tripolitania Basin (Libya) was drilled through Eocene and Oligocene deposits. Eocene sediments are predominately clayey and sandy wackestone type limestones. They contained a poor microfossil association, typical for lagoons with high salinity andweak aeration, whwre only ostracods and rare benthic foraminifea survived. At the top of Eocene a few specimens of Nummulite sp. appearwith small benthic foraminifera. In the early Oligocene gray to white packstone prevail and contain a great amount od larger benthic foraminifera.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA