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- W2000695593 abstract "Abstract Geological, mineralogical and geochemical studies were carried out on Mayouom kaolin deposit located within a mylonitic shear zone about 30 km north of Foumban town (western Cameroon), in order to define the ore genesis and its economic interest. Two facies (sandy kaolin and sand-poor kaolin) were characterised by different techniques: description of outcrops and pits, X-ray diffraction, differential scanning calorimetric and thermogravimetric analyses, scanning electron microscopy, Fourier transform infrared spectrometry and bulk chemical analyses. Sand-poor kaolin (76–85% kaolinite and 2–9% quartz) forms 1 to 2 m thick veins which crosscut sandy kaolin (48–59% kaolinite and 36–47% quartz). All the samples have the following mineral phases in common, close to an advanced argillic alteration system: kaolinite + quartz + illite/muscovite + anatase ± hematite ± Ba, Sr-hydroxyapatite ± zircon ± pyrite ± florencite. Both sandy and sand-poor kaolins present kaolinite mineral with a homogeneous shape and a good crystallinity. Results from the different analytical techniques point out a hydrothermal alteration of feldspar- and mica-rich rocks as petrogenetic origin of kaolins. Sandy kaolin comes from mylonite basement while sand-poor kaolin is related to the alteration of magmatic intrusive shape veins. Due to its high kaolinite content (up to 85%) and the low iron mineral content (" @default.
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- W2000695593 date "2006-04-01" @default.
- W2000695593 modified "2023-10-05" @default.
- W2000695593 title "Genesis of Mayouom kaolin deposit (western Cameroon)" @default.
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- W2000695593 doi "https://doi.org/10.1016/j.clay.2005.11.005" @default.
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