Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/28257
Full metadata record
DC FieldValueLanguage
dc.contributor.authorUsman, Halima Osu-
dc.contributor.authorUnuevho, Christopher Imoukhai-
dc.contributor.authorChukwuma-Orji, Jacinta Nkiru-
dc.contributor.authorAlkali, Yahaya Baba-
dc.date.accessioned2024-05-10T02:52:51Z-
dc.date.available2024-05-10T02:52:51Z-
dc.date.issued2022-11-08-
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/28257-
dc.description.abstractSequence stratigraphic analysis was carried out on well Bobo-3, deep offshore, Niger Delta Basin, Nigeria. This is done in order to delineate sequence stratigraphic units using vertical sequence of depositional environments. Palynological analysis was carried out on 82 ditch cutting samples using the standard acid technique in order to zone the studied section of the well. Open hole geophysical log data was also provided for the studied interval (10700-15600 ft) belonging to the Agbada Formation. Lithologically, the section varies from alternation of sand and shale units with carbonaceous debris, mica flakes, ferruginised materials and glauconite at some interval as accessory minerals. Palynological zonation included three taxon range zones; Belskipollis elegans, Crassoretitriletes vanraadshooveni, and Pachydermites diederixi, which Are correlatable with the pantropical biozones. The studied section is dated as early to middle Miocene based on the independent palynological evidences. The deduced paleoenvironments of the strata penetrated by the well range from outer neritic through bathyal to abyssal. The successions were differentiated into highstand systems tracts (HST), lowstand systems tracts (LST) and transgressive systems tracts (TST) and chronostratigraphic surfaces such as maximum flooding surface (MFS), sequence boundary (SB), and transgressive surface (TS). Three HST, three LST, three TST, two MFS and three SB were recognized. The MFS and SB were dated 15.9 Ma, 15.0 Ma and 16.7 Ma, 15.5 Ma, 13.1 Ma, respectively by correlation of the established pollen zones with the Niger Delta Cenozoic chronostratigraphic chart. The sandstone and shale units of the systems tracts are potential hydrocarbon reservoirs and seal rocks respectively.en_US
dc.language.isoenen_US
dc.publisherInternational Conference on the Geology of Africaen_US
dc.relation.ispartofseries11th;-
dc.subjectSequenceen_US
dc.subjectPalynozonationen_US
dc.subjectAgbada Formationen_US
dc.subjectMioceneen_US
dc.subjectNiger Deltaen_US
dc.subjectNigeriaen_US
dc.titleSequence Stratigraphic Analysis of Well Bobo-3, Deep Offshore, Niger Delta Basin, Nigeriaen_US
dc.typePresentationen_US
Appears in Collections:Geology

Files in This Item:
File Description SizeFormat 
ICGA EGYPT PPR.pdf1.45 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.