Pregled bibliografske jedinice broj: 720877
Biostratigraphy, lithology and palaeoecology of the Paleogene sediments in the two wells in Palmyra region, Syria
Biostratigraphy, lithology and palaeoecology of the Paleogene sediments in the two wells in Palmyra region, Syria // 23nd IAS Meeting of Sedimentology, Coimbra, September 15-17, 2004 : Abstracts book / Pena dos Reis, Rui ; Callapez, Pedro ; Dinis, Pedro (ur.).
Coimbra: International Association of Sedimentologists (IAS), 2004. str. 163-163 (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Biostratigraphy, lithology and palaeoecology of the Paleogene sediments in the two wells in Palmyra region, Syria
Autori
Hernitz Kučenjak, Morana ; Premec Fuček, Vlasta ; Mesić, Ivan A. ; Slavković Renata
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
23nd IAS Meeting of Sedimentology, Coimbra, September 15-17, 2004 : Abstracts book
/ Pena dos Reis, Rui ; Callapez, Pedro ; Dinis, Pedro - Coimbra : International Association of Sedimentologists (IAS), 2004, 163-163
ISBN
972-9119-25-2
Skup
23nd IAS Meeting of Sedimentology
Mjesto i datum
Coimbra, Portugal, 15.09.2004. - 17.09.2004
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Biostratigraphy; lithology; palaeocology; planktonic foraminifera; Syria
Sažetak
Jihar-1 and Jihar-2 exploration well, located in Palmyrides region in Syria, was drilled hroughout Eocene and Oligocene sediments. Results of detailed micropaleontological and lithological analyses have been carried out. The biostratigraphy of the sediment succession is analysed by means of planktonic foraminifera. As all analyses have been done from drill-cuttings, biostratigraphical boundary is based on last occurrence of the taxa. From Lower Eocene to the end of Late Eocene sedimentation took place in basinal to deep outer shelf environment. Rich and highly diversified assemblages of foraminiferal association suggest Mediterranean bioprovince with tropical to subtropical climate and open deep sea environment. Microfossil association is most diversified during Middle Eocene. In Oligocene, the most planktonic species were replaced by small benthonic foraminiferal species in according to climate change and shalowing of the sedimentation environment.
Izvorni jezik
Engleski
Znanstvena područja
Geologija