摘要
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。
Geologist found that the mic-thinsection was limited in the study of petrogenetion and sedi-mentare facies. They began to search a new methed. So the Cathodlurninescence of minerals was found. This pa-per has introduced parts of theory and results of our practice in the using and studying of cathedoluminescence inreservoir and sedimentary facies. The purpose is to make more guide for researchers in the study of reservoir andsedimentare facies.
出处
《断块油气田》
CAS
1998年第6期17-19,共3页
Fault-Block Oil & Gas Field
关键词
阴极发光
成岩作用
储集层
沉积相
油气勘探
Cathodoluminescence, Diagenesis, Reservoir evolution, Sedimentary facies
