压实作用导致原生孔隙大量损失，不稳定组分的溶解则是改善孔隙结构的主要因素。
The loss of primary porosity is caused by compaction, and pore texture reformation is resulted from the solution of unstable components.
长石的钠长石化作用和长石、岩屑的水化水解作用、溶解作用，导致了不稳定组分的转变以及大量离子游离于孔隙水中，同时导致大量的自生矿物沉淀。
The hydration-hydrolysis and dissolution rock fragments and feldspar and albitization of feldspar make many ions free from their framework and go into pore-water.
多组分填充PP显示出中等程度的出口膨胀和流动不稳定性。
The multicomponent filled PP has shown an intermediate degree of die swell and flow instabilities.
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