Weak intercalation is the main weak surface which controls the rock stability.

软弱夹层是控制岩体稳定性的主要弱面。

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The rock mass slope stability is directly influenced by mudding intercalation within the fracture zones and fault zones.

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。

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The Saliyak melange consists of dark-gray to black muddy and silty microclastic rock with intercalation of grayish purple and grayish green calcareous and muddy shale, marl and tuff.

西昆仑赛力亚克混杂堆积由形态、颜色和大小各异的沉积岩块体以及黑色泥质粉砂岩夹灰紫绿色钙质页岩、泥灰岩和层凝灰岩的基质组成。

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