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dc.creatorRostami, Leila
dc.creatorVaziri, Seyed Hamid
dc.creatorJahani, Davood
dc.creatorSolgi, Ali
dc.creatorTaherpour-Khalil-Abad, Morteza
dc.creatorCarević, Ivana
dc.creatorYahyaei, Ahmad
dc.date.accessioned2021-09-24T15:39:56Z
dc.date.available2021-09-24T15:39:56Z
dc.date.issued2018
dc.identifier.issn2228-7817
dc.identifier.urihttps://gery.gef.bg.ac.rs/handle/123456789/897
dc.description.abstractThe Dorood oilfield is located offshore in the northern part of the Persian Gulf. It partly underlies the Kharg Island. The Neocomian Fahliyan Formation represents the high-quality reservoir in the oilfield. It includes five carbonate members: The Manifa, Middle and Upper Yamama, Khami and Lower Ratawi. The Fahliyan Formation in the studied well attains a thickness of 378.1 m and mainly consists of thin-bedded limestones. It unconformably overlies the evaporate Hith Formation and conformably underlies the Gadvan Formation. An integrated biostratigraphic (benthic foraminifera and algae) and lithostratigraphic study is presented. Paleontological studies led to the identification of 19 genera and 29 species of benthic foraminifera and 10 genera and 9 species of calcareous algae. Two biozones of Berriasian through Valanginian age have been recognized. These are Lithocodium aggregatum-Salpingoporella muehlbergii assemblage zone (Valanginian) and Pseudocyclammina lituus- Coscinoconus assemblage zone (Berriasian-Valanginian).en
dc.publisherUniv Tehran, Tehran
dc.rightsrestrictedAccess
dc.sourceGeopersia
dc.subjectFahliyan Formationen
dc.subjectForaminiferaen
dc.subjectCalcareous Algaeen
dc.subjectBerriasian-Valanginianen
dc.subjectDorood Oilfielden
dc.titleBenthic foraminiferal and calcareous algal biostratigraphy of the Fahliyan Formation in oil well X1, Dorood Oilfield, Persian Gulfen
dc.typearticle
dc.rights.licenseARR
dcterms.abstractТахерпоур-Кхалил-Aбад, Мортеза; Јахани, Давоод; Солги, Aли; Царевић, Ивана; Yахyаеи, Aхмад; Вазири, Сеyед Хамид; Ростами, Леила;
dc.citation.volume8
dc.citation.issue2
dc.citation.spage319
dc.citation.epage329
dc.citation.other8(2): 319-329
dc.identifier.wos000451269600012
dc.identifier.doi10.22059/GEOPE.2018.256557.648385
dc.identifier.scopus2-s2.0-85058642780
dc.identifier.rcubhttps://hdl.handle.net/21.15107/rcub_gery_897
dc.type.versionpublishedVersion


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