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《Geological Science and Technology Information》 2008-01
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Mineralogical Characterization of Qingshuijiang Kaolin Deposit in Hepu,Guangxi

WANG Yuan1a,1b, ZHOU Han-wen1b,1c, ZENG Wei-neng2, LIAO Jin-liang2, YANG Zeng-liang2(1a.Graduate School; 1b.State Key Laboratory of Geological Processes and Mineral Resources;1c. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China; 2. Corporation of Kaolinite Science and Technology,Maoming Guangdong 525026, China)  
The paper studies the geology and genesis of Qingshuijiang kaolin deposit in Hepu, Guangxi. Kaolin mineralogy and geological data indicate that kaolinite comes from the alteration of granite pluton. Seven samples from different outcrops were analyzed on the chemical by wet method, clay mineral assemblage by XRD, and phase transformation by thermal analysis. SEM was taken for revealing the structure of the kaolin. The analysis shows that kaolin properties are related to mineralogical and chemical composition. The data obtained from the study indicate that clay mineral assemblages in this deposit vary in different areas. The quality grade for industry of the kaolin here is grade one, which can be used as the high quality raw material of paper and paint.
【CateGory Index】: P619.232
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