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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/239872
Ver los metadatos del registro completo
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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 |
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2011-01 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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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 |
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http://hdl.handle.net/11336/239872 |
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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 |
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eng |
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eng |
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info:eu-repo/semantics/altIdentifier/url/http://www.europeanjournalofscientificresearch.com |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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openAccess |
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application/pdf application/pdf |
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In Tech |
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In Tech |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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