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淮南下石盒子组球粒状高岭岩结构及成因探讨
引用本文:刘钦甫,张鹏飞.淮南下石盒子组球粒状高岭岩结构及成因探讨[J].地质科学,1995,30(4):393-400.
作者姓名:刘钦甫  张鹏飞
作者单位:中国矿业大学北京研究生部 北京 100083
摘    要:淮南下石盒子组球粒状高岭岩形成于三角洲平原上的湖泊环境。球粒是有机质与高岭石组成的复合集合体,可划分出6种结构类型。矿床中高岭石矿物主要有两种来源,一种是由陆源粘土搬运再沉积而成;另一种是由硅铝胶体沉淀并经重结晶作用而来。有机质对高岭石及球粒集合体的形成起重要作用。

关 键 词:高岭岩  结构  球粒  有机质
收稿时间:1993-11-22
修稿时间:1993-11-22;

THE TEXTURE FEATURE AND ORIGIN ANALYSIS OF PELLETOID KAOLINITE ROCK OF XIASHIHEZI FORMATION IN HUAINAN REGION
Liu Qinfu, Zhang Pengfei, Yang Xiaojie.THE TEXTURE FEATURE AND ORIGIN ANALYSIS OF PELLETOID KAOLINITE ROCK OF XIASHIHEZI FORMATION IN HUAINAN REGION[J].Chinese Journal of Geology,1995,30(4):393-400.
Authors:Liu Qinfu  Zhang Pengfei  Yang Xiaojie
Institution:Beijing Graduate School, China University of Mining and Technology, Beijing, 100083
Abstract:he kaolinite rock, 2-6 m thick, occurs 6-19 m below NO. 4 coal seam at the bottom of Xiashihezi Formation, being a stable correlation key bed in a large area. The pelletoid kaolinite rock, formed in the lacustrine environment of delta plain, is an important type of rock. Six texture types of pellets are identified: Concentric pellets without nuclei, pellets with nuclei, radial pellets, laminae-free pellets,irregular pellets, transitional pellets. Organic matter, derived from strong degradation of algae, are amorhpous and yellow-green under fluorescence, and play a great role in the formation of pellets. The clay particles suspended in the water are linked by organic matter, forming aggregates, then sinking and rolling under the influence of water current on the bottom of basin, thus forming various types of pellets. The concentric texture is also related to the seasonal change. There are two genetic kinds of kaolinite: One is the terrigenous clay minerals, transported and deposited in the lacustrine basin, which show rounded and irregular shape, The other is precipitated by alumino-silicate gels and recrystallized in the diagenesis stage, which show radial arrangment and well hexagonal flake shape.
Keywords:Kaolinite rock  Texture  Pellet  Organic matter  
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