泥化夹层是含泥质的原生软弱夹层经一系列地质作用这化面成的它多 发生在下相对坚硬而中间相对软弱刚柔相间的岩层组合条件下。在构造运动作用下产生层间错动。岩层破碎;结构改变.并为地下水渗流提供了通道。
研究结果表明：泥化夹层的水敏性强，对边坡的整体稳定性产生了较不利的影响。
The research results indicate that the effect of the Water Sensitivity of the clayer thin interlayer is strong, and the clayer thin interlay does adverse effect on stability of slope.
为此，专门制定了对K10、S63溶洞系统、溶蚀裂隙及泥化夹层的灌浆处理技术措施和方法。
The engineers specially made up grouting treatment measures and methods for solution cavities K10 and S63, solution fissures and argillation intercalations.
边坡岩体中的层间剪切破碎带、断层破碎带不同程度地赋含泥化夹层，直接影响边坡的岩体结构。
The rock mass slope stability is directly influenced by mudding intercalation within the fracture zones and fault zones.
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