Existence of karsts into silicated non-carbonated crystalline rocks in Sahelian and Equatorial Africa, hydrogeological implications
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Publication Date
7-1-2002
Publication Title
Bulletin de la Société Géologique de France
Volume Number
173
Issue Number
4
Abstract
Various cavities studied in western Niger and South Cameroon show the existence of important karstic phenomena into metagabbros and gneisses. These large-sized caves resulted from generalized dissolution of silicate formations in spite of their low solubility. Karstification is produced by deep hydrous transfer along lithological discontinuities and fracture net works. The existence of such caves has major implications in geomorphology, under either Sahelian and Equatorial climate, and in hydrogeology and water supply, particularly in the Sahel area.
Keywords
Karst, Caves, Geomorphology, Hydrogeology, Water supply
Document Type
Article
Digital Object Identifier (DOI)
https://doi.org/10.2113/173.4.337
Language
English; French
Recommended Citation
Willems, Luc; Pouclet, André; and Vicat, Jean-Paul, "Existence of karsts into silicated non-carbonated crystalline rocks in Sahelian and Equatorial Africa, hydrogeological implications" (2002). KIP Articles. 8562.
https://digitalcommons.usf.edu/kip_articles/8562
