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dc.creatorRami, Mahin
dc.creatorVaziri, Mohammad Reza
dc.creatorAbad, Morteza Taherpour Khalil
dc.creatorHosseini, Seyed Abolfazl
dc.creatorCarević, Ivana
dc.creatorAllameh, Mohsen
dc.date.accessioned2021-09-24T15:24:22Z
dc.date.available2021-09-24T15:24:22Z
dc.date.issued2012
dc.identifier.issn1026-8774
dc.identifier.urihttps://gery.gef.bg.ac.rs/handle/123456789/488
dc.description.abstractThe Barremian-Aptian sediments in the Bararig section (Southwest of Kuhbanan) consist of fan alternation of marl and limestone. The palaeontological analysis led to identification of twenty seven taxa of benthic foraminifera and algae in the section studied. Diverse assemblages of benthic foraminifera and also the low planktonic/benthic (P/B) ratio show that the sedimentary environment in the study area was oxygenated and shallow.en
dc.publisherUniversidad Nacional Autónoma de México
dc.rightsopenAccess
dc.sourceRevista Mexicana de Ciencias Geologicas
dc.subjectmicrobiostratigraphyen
dc.subjectpalaeoecologyen
dc.subjectLower Cretaceousen
dc.subjectBararig sectionen
dc.subjectKerman Provinceen
dc.subjectIranen
dc.titleMicrobiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iranen
dc.typearticle
dc.rights.licensePublisher's own license
dcterms.abstractЦаревић, Ивана; Рами, Махин; Вазири, Мохаммад Реза; Хоссеини, Сеyед Aболфазл; Aлламех, Мохсен; Aбад, Мортеза Тахерпоур Кхалил;
dc.citation.volume29
dc.citation.issue1
dc.citation.spage63
dc.citation.epage75
dc.citation.other29(1): 63-75
dc.citation.rankM23
dc.identifier.wos000302822900004
dc.identifier.scopus2-s2.0-84866884006
dc.identifier.rcubhttps://hdl.handle.net/21.15107/rcub_gery_488
dc.type.versionpublishedVersion


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