The diagenetic environment results in different water-rock reaction and development of secondary porosity. 成巖環(huán)境在一定程度上影響了水巖反應及次生孔隙發(fā)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. 由于成巖環(huán)境的變化常與構造運動(dòng)有關(guān)，因此膠結物地層學(xué)的研究可以間接地分析構造運動(dòng)發(fā)生的時(shí)期。
