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《GEOCHIMICA》 1999-03
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Clay mineral, chemical characteristics and environmental record of the Multi stage laterite at Yingfengling Section, Leizhou Peninsula

Xu Yifang Zhu Zhaoyu Wen Qizhong Wen Gaoguo Pu Zhiping(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)  
The results of mineral and chemical analyses indicate that the multi stage laterite formed in the early lateritization stage of basalts of Yingfengling, Leizhou Peninsula of Guangdong Province. The laterite maturity gradually increases from the bottom to the top of the lateritic section. The clay mineral contents in the laterite, Fe2O3 contents in the clay and chemical indexes, such as oxidation, eluviation, ferrite and aluminum enrichment vary with the section depth. That is resulted from pedogenic environmental variations caused by climatic alteration and volcanic effect. This result indicates that at least 9 pedogenic environmental variations were recorded in the laterite volcanic rock section of Yingfengling.
【Fund】: 广东省自然科学基金!( 编号:963206);;国家自然科学基金!( 编号:49772138) ;;“九五”国家重大基金!( 编号:498
【CateGory Index】: P588.241
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