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葛洲坝泥化夹层的物质组成特性
引用本文:谭罗荣.葛洲坝泥化夹层的物质组成特性[J].岩土力学,1984,5(2):27-34.
作者姓名:谭罗荣
摘    要:葛溯坝基岩中,砂岩或粉砂岩岩层间夹有一些厚薄不等,性状各异的粘土岩或粉砂质粘土岩,以及它们的泥化夹层等软弱夹层。本文主要是根据若干典型夹层的矿物成分及其定量分析结果和部分颗粒分析资料等,叙述和讨论了软弱岩层的物质组成,特别是亲水性粘土矿物的组成特性与泥化夹层形成的关系。

关 键 词:粘土矿物    泥化夹层    粉砂质    定量分析结果    构造应力作用    粘土岩    岩性变化    层位    典型剖面    矿物成分  

The Behaviour of Weak Intercalations Compositions of Matter at Gezhouba Dam
Tan Luorong.The Behaviour of Weak Intercalations Compositions of Matter at Gezhouba Dam[J].Rock and Soil Mechanics,1984,5(2):27-34.
Authors:Tan Luorong
Abstract:In the base rock of the Gezhouba Dam between sandstones, and siltstones there are A number of weak intercalations consisting of claystones, silty-claystones, and their argillitgation intercalation with different thickness and behavior. Base on the results of the Quantitatire analyses of the mineral compositions and some data of grani size analysis on some representative interactions, the relation between the composition of weak intercalation, especially hydrophilic clay mineral composition, and the formation of argilligation intercalations is described and researched.
Keywords:
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