@article{fdi:010057214, title = {{G}eological study of sedimentary clayey materials of the {B}omkoul area in the {D}ouala region ({D}ouala sub-basin, {C}ameroon) for the ceramic industry}, author = {{N}gon, {G}. {F}. {N}. and {E}tame, {J}. and {N}tamak-{N}ida, {M}. {J}. and {M}bog, {M}. {B}. and {M}pondo, {A}. {M}. {M}. and {G}{\'e}rard, {M}artine and {Y}ongue-{F}ouateu, {R}. and {B}ilong, {P}.}, editor = {}, language = {{ENG}}, abstract = {{A} geological study carried out in the {B}omkoul area ({D}ouala sub-basin, {C}ameroon) has revealed the presence of heterogeneous clayey materials on hills (80-120 m altitude). {T}he clay deposits are thick at the upper slope where sandstones and sandy-clay overlying clay layers, and thin at the middle and lower slopes where weathered clays overlying clay layers. {C}layey materials identified are grey, dark-grey and mottled in color, with sandy-clay, clayey-silt, silty-clay and clay textures. {R}aw materials are mostly made up of fine particles ranging from 52 to 82% clay and silt in the mottled clayey material, 50 to 82% clay and silt in the dark-grey clayey material and 70 to 85% in the grey clayey material. {T}heir chemical composition is characterized by silica (<70% {S}i{O}2), alumina (<32% {A}l2{O}3) and iron (1 to 16% {F}e2{O}3). {T}he main clay minerals are disorganized and poorly crystallized kaolinite and few smectite. {T}he physical, mineralogical and geochemical properties of these materials presented and discussed in this work show that the clayey raw materials of the {B}omkoul area have a good potential for pottery as well as brick, tile and soil sandstone manufacture.}, keywords = {{C}layey material ; {K}aolinite ; {S}mectite ; {L}ocal material ; {B}omkoul ; {D}ouala sub-basin ; {C}ameroon}, booktitle = {}, journal = {{C}omptes {R}endus {G}eoscience}, volume = {344}, numero = {6-7}, pages = {366--376}, ISSN = {1631-0713}, year = {2012}, DOI = {10.1016/j.crte.2012.05.004}, URL = {https://www.documentation.ird.fr/hor/fdi:010057214}, }