摘要
总结了塔中隆起石炭系CⅠ油组石英砂岩储集层的压实、压溶、胶结、溶解、交代作用等成岩特征,划分出准同生期、早成岩A期和B期、晚成岩A期和B期五个成岩阶段,通过成岩机理的分析,提出本区成岩环境是一个半封闭到封闭的系统,建立了成岩模式,并讨论了成岩作用的影响因素及其与储集性能的关系。
This paper summarized the diagenetic features of CⅠ oil group quartzose sandstone reservoir of Carboniferous system in Tazhong uplift, such as compaction and pressure solution, cementation, dissolution, alteration and replacement. Five stages of diagenesis were classified, including penecontemporaneous, early diagenetic stage A and B, late diagenetic stage A and telodiagenetic stage B. By analysis of the diagenetic mechanisms, furthermore, diagenetic mode is established. For the first time, it is pointed out that the diagenetic environment in this region was a semi sealed to sealed system. Factors affecting the diagenesis and their relations to reservoir quality of CⅠ oil group are discussed.
出处
《新疆石油地质》
CAS
CSCD
1998年第5期388-392,400,共6页
Xinjiang Petroleum Geology
关键词
塔里木盆地
中石炭世
油矿床
储集层
成岩模式
Tarim Basin Middle Middle Carboniferous Sandstone Diagenesis Mode Reservoir Characteristics