The diagenetic environment results in different water-rock reaction and development of secondary porosity. 成岩环境在一定程度上影响了水岩反应及次生孔隙发育。
As change of diagenetic environments is commonly related with structural movements, time of structural movement can also be inferred through the study of cement stratigraphy. 由于成岩环境的变化常与构造运动有关，因此胶结物地层学的研究可以间接地分析构造运动发生的时期。
