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不规则伊/蒙混层粘土矿物成因类型及晶体化学分类
引用本文:陆琦,雷新荣,刘惠芳.不规则伊/蒙混层粘土矿物成因类型及晶体化学分类[J].矿物学报,1991(2).
作者姓名:陆琦  雷新荣  刘惠芳
作者单位:中国地质大学,中国地质大学,中国地质大学 武汉 430074,武汉 430074,武汉 430074
基金项目:国家自然科学基金,编号4880082
摘    要:不规则伊/蒙混层粘土矿物(I/S)分布极为广泛,根据大量资料,提出了I/S的成因及晶体化学分类。按其成因分为三类:成岩型、风化型、火山热液型;按其晶体化学性质分为完全无序型、部分有序型及准晶态型。讨论了各成因类型I/S的晶体化学特点,认为产出于P/T界线层粘土中的I/S具二维晶格一维准晶格。探讨了I/S与烃类形成的关系。

关 键 词:伊/蒙混层粘土矿物  成因类型  晶体化学  准晶态

GENETIC TYPES AND CRYSTALLOCHEMICAL CLASSIFICATION OF IRREGULAR ILLITE/SMECTITE INTERSTRATIFIED CLAY MINERALS
Lu Qi Lei Xinrong Liu Huifang.GENETIC TYPES AND CRYSTALLOCHEMICAL CLASSIFICATION OF IRREGULAR ILLITE/SMECTITE INTERSTRATIFIED CLAY MINERALS[J].Acta Mineralogica Sinica,1991(2).
Authors:Lu Qi Lei Xinrong Liu Huifang
Abstract:Irregular illite/smectite interstratified clay minerals (I/S)are widespread in nature. Based on the available data, we have proposed the genetic types and crystallochemical classification. I/S can be genetically grouped into three types: diagenetic, weathered, and volcano-hydrothermal.Crystallochemically, I/S can be classified as three groups: fully random, partly regular, and quasicrystal. Studies of the crystallochemical properties of every genetic type of I/S show that the I/S found in the P/T boundary clay layer exhibits twodimensional crystal and one-dimensional quasicrystal structures. The relationship between I/S and hydro-carbon-formaton has also been discussed.
Keywords:irregular illite/smectite interstratified clay mineral  genetic type  crystallochemical classification  quasicrystal structure  
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