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国内外深部优质储层的不断发现大大拓宽了油气勘探的新领域，但孔隙流体自然排放的压实理论和有机无机反应的次生孔隙窗机理对深部高孔渗储层并不能作出圆满解释。深部储层孔隙保存状况除与储层物质组成及其内部结构有关外，与各成岩动力学过程间的耦合关系更为密切。压实作用、胶结作用、粘土矿物转化、有机质热演化、溶蚀作用、异常流体压力的积累与释放等动力学过程在时间和空间上的不同组合决定了深部储层孔隙的发育程度及其保存状况。
The continuous discovery of deep high-quality reservoirs at home and abroad has greatly broadened the exploration of oil and gas fields. However, the compaction theory of natural pore fluid discharge and the secondary pore-window mechanism of organic-inorganic reactions can not provide a satisfactory explanation for the deep percolation reservoirs. In addition to the reservoir material composition and its internal structure, the reservoir porosity in deep reservoirs is more closely related to each diagenetic kinetic process. The different combination of time and space dynamics process of compaction, cementation, conversion of clay minerals, thermal evolution of organic matter, dissolution, accumulation and release of abnormal fluid pressure determine the development degree and preservation status of deep reservoir pores .