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dc.contributor.authorMomo, M.N.
dc.contributor.authorYemefack, M.
dc.contributor.authorTematio, P.
dc.contributor.authorBeauvais, A.
dc.contributor.authorAmbrosi, J.
dc.date.accessioned2019-12-04T10:57:28Z
dc.date.available2019-12-04T10:57:28Z
dc.date.issued2016-05-01
dc.identifier.citationMomo, M. N., Yemefack, M., Tematio, P., Beauvais, A., & Ambrosi, J. P. (2016). Distribution of duricrusted bauxites and laterites on the Bamiléké plateau (West Cameroon): constraints from GIS mapping and geochemistry. CATENA, 140, 15-23.
dc.identifier.issn0341-8162
dc.identifier.urihttps://hdl.handle.net/20.500.12478/748
dc.description.abstractEstimation of the mineral resources potential is an important issue for most of developing countries. The spatial distribution of bauxites and lateritic land surfaces on the Bamiléké plateau (West Cameroon) has been investigated with a Boolean modeling process into a GIS environment on the basis of geological constraints such as elevation, rock and soil types, and landscape morphology. Field observation and SRTM (Shuttle Radar Topographic Mission) data allowed the differentiation of two lateritic land surfaces separated by a minimum altitude difference of about 60 m. These surfaces constrained by favorable rock types, slope steepness and soil types provided a potential lateritic bauxitic area of 381 km2 (17.2% of the total study site). Field validation and the integration of legacy spatial data resulted in an area of 60.1 km2 for potential bauxitic ores, i.e. obviously duricrusted bauxitic surfaces (with 47.8 km2 in the upper surface and 12.3 km2 in the lower surface). Alumina contents obtained from duricrust samples were analyzed by geostatistical methods and classical kriging interpolation to discriminate between bauxitic and ferruginous laterites. This highlighted a geochemical trend from higher alumina values on the upper surface (40–66 wt.%) to lower values on the lower surface (13–44 wt.%). Finally, our study documents two duricrusted lateritic surfaces arranged in a staircase manner and having different geochemical characteristics. The total bauxitic-rich surface is distributed in five spots throughout the study area and covers 56.2 km2, while ferruginous laterites occupy a spot of 3.9 km2. GIS mapping approach of lateritic land surfaces, accounting for reliable constraints, might be promising for larger scale investigations of mineral resources in Cameroon.
dc.format.extent15-23
dc.language.isoen
dc.subjectGis
dc.subjectGeochemistry
dc.subjectFerrasols
dc.subjectLaterite
dc.titleDistribution of duricrusted bauxites and laterites on the Bamiléké plateau (West Cameroon): constraints from GIS mapping and geochemistry
dc.typeJournal Article
dc.description.versionPeer Review
cg.contributor.crpWater, Land and Ecosystems
cg.contributor.affiliationUniversité de Dschang
cg.contributor.affiliationInstitut de Recherche Agricole pour le Développement, Cameroon
cg.contributor.affiliationInternational Institute of Tropical Agriculture
cg.contributor.affiliationUniversité d'Aix-Marseille
cg.coverage.regionAfrica
cg.coverage.regionWest Africa
cg.coverage.countryCameroon
cg.isijournalISI Journal
cg.authorship.typesCGIAR and developing country institute
cg.iitasubjectSoil Information
cg.journalCatena
cg.howpublishedFormally Published
cg.accessibilitystatusLimited Access
local.dspaceid72856
cg.targetaudienceScientists
cg.identifier.doihttps://dx.doi.org/10.1016/j.catena.2016.01.010


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