由于成岩作用不同，粘土的分布形式呈多样化，如丝状和覆盖在骨架颗粒表面的粘土膜。

We can make several conclusions as following: a The distributing shape is various because of different ore-forming processes.

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通过加电前后岩石颗粒的粒度测定试验，研究了外加电场对岩石骨架颗粒和粘土矿物性质的影响。

This paper tries to study how the externally applied electric field influence the properties of rock grain and clay minerals, by testing the grain size before and after applying electric current.

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而在松散沉积物实验中，水合物先依附于沉积物骨架生成，并胶结了骨架颗粒，之后水合物开始在沉积物孔隙中以悬浮状形态生成。

However gas hydrate is formed firstly on the skeleton and cement the granules in unconsolidated sediments experiments, afterward they grow suspending in the pore space.

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