MORPHOLOGICAL TRANSFORMATION OF KAOLIN MINERALS FROM GRANITE SAPROLITE IN THE WESTERN PART OF CAMEROON
スポンサーリンク
概要
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The weathering process of a granitic rock was mineralogically investigated with XRD, XRF, SEM and TEM at one weathered profile (Ca. 20m in height) in the western part of Cameroon where climate is the intermediate of humid and arid tropical condition. Halloysite and kaolinite are main constituent clay minerals in the granite saprolite (weathered granite). Halloysite predominantly occurs at the lower part of the investigated profile associating with small amount of kaolinite. Numerous spherical-shaped halloysite were observed in the bottom of the profile under TEM. The granite saprolite at the top part of the profile consists mainly of platy kaolinite with small amount of tubular halloysite. Detailed observation of morphological variation by TEM together with X-ray analysis revealed that the spherical-shaped halloysite crystals (0.05-0.5μm) are first unrolled and then transform to tubular halloysite (0.05-2μm), and finally unrolled again producing platy kaolinite (0.2-3μm). Close relationship between crystal size and morphology is obtained.
- 日本粘土学会の論文
著者
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KITAGAWA RYUJI
Department of Earth and Planetary System Science, Hiroshima University
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Kitagawa R
Department Of Earth And Planetary Sciences Faculty Of Science Hiroshima University
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Kitagawa Ryuji
Department Of Earth And Planetary Sciences Graduate School Of Science Hiroshima University
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Wouatong Armand
Department Of Earth Science Faculty Of Science University Of Dschang
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TAKENO SETSUO
Department of Earth and Planetary Sciences, Faculty of Science, Hiroshima University
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TCHOUA FELIX
Department of Earth Sciences, Faculty of Science, University of Yaounde
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NJOPWOUO DANIEL
Department of inorganic chemistry, Faculty of Science, University of Yaounde
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Tchoua Felix
Department Of Earth Sciences Faculty Of Science University Of Yaounde
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Takeno Setsuo
Department Of Earth And Planetary Sciences Faculty Of Science Hiroshima University
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Njopwouo Daniel
Department Of Inorganic Chemistry Faculty Of Science University Of Yaounde
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Wouatong Armand
Department Of Earth And Planetary Sciences Faculty Of Science Hiroshima University
関連論文
- THE OCCURRENCE AND STRUCTURE OF VERMIFORM CHLORITE
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- CLAY MINERALOGY OF THE LANDSLIDE IN LEMBO AREA, BANA-BANGOU DISTRICT, WEST PROVINCE OF CAMEROON
- MORPHOLOGICAL TRANSFORMATION OF KAOLIN MINERALS FROM GRANITE SAPROLITE IN THE WESTERN PART OF CAMEROON
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