Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria

The methods of seismic geohistory analysis and differential interformational velocity analysis have been applied using datafrom some interpreted seismic sections within the Anambra basin. These two techniques for basin analysis have been appliedin the basin in an attempt to aid the identification of...

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Autores:
A.S, Ekine
K. M, Onuoha,
Tipo de recurso:
Article of journal
Fecha de publicación:
2010
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/33918
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/33918
http://bdigital.unal.edu.co/23998/
http://bdigital.unal.edu.co/23998/2/
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Atribución-NoComercial 4.0 Internacional
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spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2A.S, Ekinec35b8850-165e-4b9b-8542-864637e151c2300K. M, Onuoha,12a47872-ecf9-422d-870c-514eef87b6ad3002019-06-27T23:06:52Z2019-06-27T23:06:52Z2010https://repositorio.unal.edu.co/handle/unal/33918http://bdigital.unal.edu.co/23998/http://bdigital.unal.edu.co/23998/2/The methods of seismic geohistory analysis and differential interformational velocity analysis have been applied using datafrom some interpreted seismic sections within the Anambra basin. These two techniques for basin analysis have been appliedin the basin in an attempt to aid the identification of anomalous velocity zones. Results from the seismic geohistory analysis indicatethat some faults arising probably from compressional stresses, due to the upliftment of the Abakaliki anticlinorium, were observed to be significant mostly in the northern and southeastern regions of the basin. These faults which originated in the Santonian are probably related to the first folding episode in the evolution of the Benue Trough. The Maestrichtian / Campanian faults observed towards the north of Anambra River-3 well may also have been influenced by these stresses or are directly related to the Post-Maestrichtian folding episode in the Benue Trough. The fault system KP identified on the seismic section is a Pre-Eocene event which cuts across from the south of Okpo-1 and Nzam-1 to the north of Iji-1 well. Sediments to the north of Nzam-1 well site have experienced more faulting during the Lower-Maestrichtian times. Fault systems that occurred after the Paleocene times are more prominent in the southern parts of Nzam-1 towards Iji-1 well sites. Generally most ofthe major faults occurred in the Paleocene. The major 'DIVA' anomaly observed southeast of Anambra River-1 well correlateswith the zone of overpressures within which liquid hydrocarbon, water and gas have been discovered in the basin. The Maestrichtian to Paleocene sediments in the southern and mainly in the southwestern sector of the Anambra basin should be the major sedimentary strata with liquid hydrocarbon potentials, whereas the Lower Cretaceous and particularly the Santonian sediments exhibit the highest potentials for gaseous hydrocarbons.application/pdfspaUNIVERSIDAD NACIONAL DE COLOMBIAhttp://revistas.unal.edu.co/index.php/esrj/article/view/21096Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalEarth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 2339-3459 1794-6190A.S, Ekine and K. M, Onuoha, (2010) Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria. Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 2339-3459 1794-6190 .Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeriaArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINAL21096-71505-1-PB.pdfapplication/pdf2566754https://repositorio.unal.edu.co/bitstream/unal/33918/1/21096-71505-1-PB.pdffe2909f2926d93c82f01af43b627431fMD51THUMBNAIL21096-71505-1-PB.pdf.jpg21096-71505-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg7512https://repositorio.unal.edu.co/bitstream/unal/33918/2/21096-71505-1-PB.pdf.jpg5b4f1c392908c8bbdbc2d1d6b5111120MD52unal/33918oai:repositorio.unal.edu.co:unal/339182022-12-28 23:03:33.396Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co
dc.title.spa.fl_str_mv Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
title Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
spellingShingle Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
title_short Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
title_full Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
title_fullStr Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
title_full_unstemmed Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
title_sort Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria
dc.creator.fl_str_mv A.S, Ekine
K. M, Onuoha,
dc.contributor.author.spa.fl_str_mv A.S, Ekine
K. M, Onuoha,
description The methods of seismic geohistory analysis and differential interformational velocity analysis have been applied using datafrom some interpreted seismic sections within the Anambra basin. These two techniques for basin analysis have been appliedin the basin in an attempt to aid the identification of anomalous velocity zones. Results from the seismic geohistory analysis indicatethat some faults arising probably from compressional stresses, due to the upliftment of the Abakaliki anticlinorium, were observed to be significant mostly in the northern and southeastern regions of the basin. These faults which originated in the Santonian are probably related to the first folding episode in the evolution of the Benue Trough. The Maestrichtian / Campanian faults observed towards the north of Anambra River-3 well may also have been influenced by these stresses or are directly related to the Post-Maestrichtian folding episode in the Benue Trough. The fault system KP identified on the seismic section is a Pre-Eocene event which cuts across from the south of Okpo-1 and Nzam-1 to the north of Iji-1 well. Sediments to the north of Nzam-1 well site have experienced more faulting during the Lower-Maestrichtian times. Fault systems that occurred after the Paleocene times are more prominent in the southern parts of Nzam-1 towards Iji-1 well sites. Generally most ofthe major faults occurred in the Paleocene. The major 'DIVA' anomaly observed southeast of Anambra River-1 well correlateswith the zone of overpressures within which liquid hydrocarbon, water and gas have been discovered in the basin. The Maestrichtian to Paleocene sediments in the southern and mainly in the southwestern sector of the Anambra basin should be the major sedimentary strata with liquid hydrocarbon potentials, whereas the Lower Cretaceous and particularly the Santonian sediments exhibit the highest potentials for gaseous hydrocarbons.
publishDate 2010
dc.date.issued.spa.fl_str_mv 2010
dc.date.accessioned.spa.fl_str_mv 2019-06-27T23:06:52Z
dc.date.available.spa.fl_str_mv 2019-06-27T23:06:52Z
dc.type.spa.fl_str_mv Artículo de revista
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http://bdigital.unal.edu.co/23998/2/
url https://repositorio.unal.edu.co/handle/unal/33918
http://bdigital.unal.edu.co/23998/
http://bdigital.unal.edu.co/23998/2/
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dc.relation.spa.fl_str_mv http://revistas.unal.edu.co/index.php/esrj/article/view/21096
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal
Earth Sciences Research Journal
dc.relation.ispartofseries.none.fl_str_mv Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 2339-3459 1794-6190
dc.relation.references.spa.fl_str_mv A.S, Ekine and K. M, Onuoha, (2010) Seismic geohistory and differential interformational velocity analysis in the anambra basin, nigeria. Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 Earth Sciences Research Journal; Vol. 14, núm. 1 (2010); 88-99 2339-3459 1794-6190 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
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dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
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