On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa

Autores
Zeli Digbehi, Bruno; Marfil, Silvina; Maiza, Pedro Jose; Goah, Bie; Mondé, Sylvain; Boko Sombo, Célestin; Wognin, Ama Valérie
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We studied the argillaceous fractions of three wells carried out in Samo area, located in the South-Eastern part of Côte d’Ivoire sedimentary basin. Preliminary works whose results are presented in this paper related to the mineralogical studies of clays of the levels crossed by these wells. They precede the study aiming at establishing the palynostratigraphy as well as the variation of the depositional environments in connection with the eustatic episodes which occurred in this sector of the Northern Gulf of Guinea. The results indicate that analyzed samples are mainly made up of quartz and kaolinite with a small proportion of illite. In the upper part sequence identified like the Continental terminal, the deposits are primarily made up of quartz and kaolinite. In bituminous gray clays of the lower section, the samples are dominated by quartz and illite. These results lead to distinguish two lithostratigraphical sequences: the variegated clays of Continental terminal Mio-Pliocene age are provided by Quaternary lateritic continental detritus; the Lower sequence of bituminous clays is mainly marine origin.
Fil: Zeli Digbehi, Bruno. Université de Cocody; Francia
Fil: Marfil, Silvina. Universidad Nacional del Sur; Argentina
Fil: Maiza, Pedro Jose. Universidad Nacional del Sur; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca; Argentina
Fil: Goah, Bie. Université de Cocody; Francia
Fil: Mondé, Sylvain. Université de Cocody; Francia
Fil: Boko Sombo, Célestin. Université de Cocody; Francia
Fil: Wognin, Ama Valérie. Université de Cocody; Francia
Materia
Shales
Tertiary
Samo,
Côte d'Ivoire
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/239872

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network_name_str CONICET Digital (CONICET)
spelling On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West AfricaZeli Digbehi, BrunoMarfil, SilvinaMaiza, Pedro JoseGoah, BieMondé, SylvainBoko Sombo, CélestinWognin, Ama ValérieShalesTertiarySamo,Côte d'Ivoirehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We studied the argillaceous fractions of three wells carried out in Samo area, located in the South-Eastern part of Côte d’Ivoire sedimentary basin. Preliminary works whose results are presented in this paper related to the mineralogical studies of clays of the levels crossed by these wells. They precede the study aiming at establishing the palynostratigraphy as well as the variation of the depositional environments in connection with the eustatic episodes which occurred in this sector of the Northern Gulf of Guinea. The results indicate that analyzed samples are mainly made up of quartz and kaolinite with a small proportion of illite. In the upper part sequence identified like the Continental terminal, the deposits are primarily made up of quartz and kaolinite. In bituminous gray clays of the lower section, the samples are dominated by quartz and illite. These results lead to distinguish two lithostratigraphical sequences: the variegated clays of Continental terminal Mio-Pliocene age are provided by Quaternary lateritic continental detritus; the Lower sequence of bituminous clays is mainly marine origin.Fil: Zeli Digbehi, Bruno. Université de Cocody; FranciaFil: Marfil, Silvina. Universidad Nacional del Sur; ArgentinaFil: Maiza, Pedro Jose. Universidad Nacional del Sur; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca; ArgentinaFil: Goah, Bie. Université de Cocody; FranciaFil: Mondé, Sylvain. Université de Cocody; FranciaFil: Boko Sombo, Célestin. Université de Cocody; FranciaFil: Wognin, Ama Valérie. Université de Cocody; FranciaIn Tech2011-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/239872Zeli Digbehi, Bruno; Marfil, Silvina; Maiza, Pedro Jose; Goah, Bie; Mondé, Sylvain; et al.; On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa; In Tech; European Journal of Scientific Research; 50; 2; 1-2011; 270-2831450-216XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.europeanjournalofscientificresearch.cominfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-02-26T10:25:37Zoai:ri.conicet.gov.ar:11336/239872instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982026-02-26 10:25:37.654CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
title On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
spellingShingle On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
Zeli Digbehi, Bruno
Shales
Tertiary
Samo,
Côte d'Ivoire
title_short On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
title_full On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
title_fullStr On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
title_full_unstemmed On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
title_sort On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa
dc.creator.none.fl_str_mv Zeli Digbehi, Bruno
Marfil, Silvina
Maiza, Pedro Jose
Goah, Bie
Mondé, Sylvain
Boko Sombo, Célestin
Wognin, Ama Valérie
author Zeli Digbehi, Bruno
author_facet Zeli Digbehi, Bruno
Marfil, Silvina
Maiza, Pedro Jose
Goah, Bie
Mondé, Sylvain
Boko Sombo, Célestin
Wognin, Ama Valérie
author_role author
author2 Marfil, Silvina
Maiza, Pedro Jose
Goah, Bie
Mondé, Sylvain
Boko Sombo, Célestin
Wognin, Ama Valérie
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv Shales
Tertiary
Samo,
Côte d'Ivoire
topic Shales
Tertiary
Samo,
Côte d'Ivoire
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv We studied the argillaceous fractions of three wells carried out in Samo area, located in the South-Eastern part of Côte d’Ivoire sedimentary basin. Preliminary works whose results are presented in this paper related to the mineralogical studies of clays of the levels crossed by these wells. They precede the study aiming at establishing the palynostratigraphy as well as the variation of the depositional environments in connection with the eustatic episodes which occurred in this sector of the Northern Gulf of Guinea. The results indicate that analyzed samples are mainly made up of quartz and kaolinite with a small proportion of illite. In the upper part sequence identified like the Continental terminal, the deposits are primarily made up of quartz and kaolinite. In bituminous gray clays of the lower section, the samples are dominated by quartz and illite. These results lead to distinguish two lithostratigraphical sequences: the variegated clays of Continental terminal Mio-Pliocene age are provided by Quaternary lateritic continental detritus; the Lower sequence of bituminous clays is mainly marine origin.
Fil: Zeli Digbehi, Bruno. Université de Cocody; Francia
Fil: Marfil, Silvina. Universidad Nacional del Sur; Argentina
Fil: Maiza, Pedro Jose. Universidad Nacional del Sur; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca; Argentina
Fil: Goah, Bie. Université de Cocody; Francia
Fil: Mondé, Sylvain. Université de Cocody; Francia
Fil: Boko Sombo, Célestin. Université de Cocody; Francia
Fil: Wognin, Ama Valérie. Université de Cocody; Francia
description We studied the argillaceous fractions of three wells carried out in Samo area, located in the South-Eastern part of Côte d’Ivoire sedimentary basin. Preliminary works whose results are presented in this paper related to the mineralogical studies of clays of the levels crossed by these wells. They precede the study aiming at establishing the palynostratigraphy as well as the variation of the depositional environments in connection with the eustatic episodes which occurred in this sector of the Northern Gulf of Guinea. The results indicate that analyzed samples are mainly made up of quartz and kaolinite with a small proportion of illite. In the upper part sequence identified like the Continental terminal, the deposits are primarily made up of quartz and kaolinite. In bituminous gray clays of the lower section, the samples are dominated by quartz and illite. These results lead to distinguish two lithostratigraphical sequences: the variegated clays of Continental terminal Mio-Pliocene age are provided by Quaternary lateritic continental detritus; the Lower sequence of bituminous clays is mainly marine origin.
publishDate 2011
dc.date.none.fl_str_mv 2011-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/239872
Zeli Digbehi, Bruno; Marfil, Silvina; Maiza, Pedro Jose; Goah, Bie; Mondé, Sylvain; et al.; On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa; In Tech; European Journal of Scientific Research; 50; 2; 1-2011; 270-283
1450-216X
CONICET Digital
CONICET
url http://hdl.handle.net/11336/239872
identifier_str_mv Zeli Digbehi, Bruno; Marfil, Silvina; Maiza, Pedro Jose; Goah, Bie; Mondé, Sylvain; et al.; On the Absence of Oligocene in Onshore Part of Cote D’ivoire Sedimentary Basin. Preliminary Results of Clays Study of Samo Area, South-East of Cote D’ivoire, West Africa; In Tech; European Journal of Scientific Research; 50; 2; 1-2011; 270-283
1450-216X
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.europeanjournalofscientificresearch.com
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv In Tech
publisher.none.fl_str_mv In Tech
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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