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目的：探索储层成岩作用和沉积相研究新方法。方法：根据阴极发光原理，结合前人工作经验和部分理论成果，阐述石英、长石及碳酸盐三种主要造岩矿物的不同阴极发光特点及其相对应的地质条件。结果：总结出不同成岩过程中矿物阴极发光特征的变化规律和不同介质环境下的碳酸盐阴极发光特征，依此可确定不同成岩作用阶段的沉积相特征。结论：利用阴极发光技术进行储层地质研究已初见成效，有待进一步推广应用。
Objective: To explore new methods of reservoir diagenesis and sedimentary facies research. Methods: According to the principle of cathodoluminescence, combined with the previous work experience and some theoretical achievements, the different cathodoluminescence characteristics of quartz, feldspar and carbonate rock minerals and their corresponding geological conditions were expounded. Results: The variation law of the cathodoluminescence of the minerals in different diagenetic processes and the characteristics of cathodoluminescence of carbonate cathodes under different media environments were summarized, and the characteristics of sedimentary facies at different diagenetic stages were determined. Conclusion: The study of reservoir geology by using cathodoluminescence has achieved initial success and needs to be further popularized.