Pregled bibliografske jedinice broj: 750129
Biostratigraphical, lithological and paleoecological aspects of the Late Cretaceous (Maastrichtian) and Paleogene sediments in the Jihar-1 well (Palmyra region, Syria)
Biostratigraphical, lithological and paleoecological aspects of the Late Cretaceous (Maastrichtian) and Paleogene sediments in the Jihar-1 well (Palmyra region, Syria) // Abstracts book of the 22nd IAS Meeting of Sedimentology / Vlahović, Igor (ur.).
Zagreb: Hrvatski geološki institut, 2003. str. 79-79 (poster, nije recenziran, sažetak, znanstveni)
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Naslov
Biostratigraphical, lithological and paleoecological aspects of the Late Cretaceous (Maastrichtian) and Paleogene sediments in the Jihar-1 well (Palmyra region, Syria)
Autori
Hernitz Kučenjak, Morana ; Premec-Fuček, Vlasta ; Stanković, Damir ; Mesić, Ivan, A. ; Benić, Josip
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Abstracts book of the 22nd IAS Meeting of Sedimentology
/ Vlahović, Igor - Zagreb : Hrvatski geološki institut, 2003, 79-79
Skup
22nd IAS Meeting of Sedimentology
Mjesto i datum
Opatija, Hrvatska, 17.09.2003. - 19.09.2003
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
planktonic foraminera; Maastrichtian; Paleogene; Syria
Sažetak
Jihar-1 exploration well, located in Palmyrides region in Syria, was drilled throughout Late Cretaceous (Maastri-chtian) and Paleogene sediments. Results of detailed micro- paleontological and lithological analyses have been carried out. The biostratigraphy of the sediment succesion is analysed by means of planktonic foraminifera and calcare-ous nannoplankton. From Late Cretaceous to the end of Late Eocene sedimentation took place in basinal to deep outer shelf environment. Rich and highly diversified assemblages of foraminiferal and calcareous nanoplankton association suggest Mediterranean bioprovince with tropical to sub-tropical climate and deep open shelf to upper bathyal envi-ronment. Microfossil association is most diversified during Upper Cretaceous and Middle Eocene. In Oligocene, plank-tonic species were replaced by small benthic foraminiferal species in according to climate change and shallowing of the sedimentary environment.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Profili:
Josip Benić
(autor)
Morana Hernitz Kučenjak
(autor)
Vlasta Premec-Fuček
(autor)
Ivan Mesić
(autor)