摘要
本文根据碳酸盐岩成岩特性,结合四川盆地地质构造、沉积特征、油气演化史及勘探实践,论述二、三叠系及石炭系的异常高压,是上覆地层静压力和油气生成、运移、聚集过程中各种地质综合作用造成的。
The author of this paper describes the anomaly high-pressure in the Triassic and the Permo-Carboniferous systems based on the features of the carbonate diagenesis combined with the geological structures, sedimentary characters, petroleum evolution and the exploration practice in the Sichuan Basin. It is concluded that the high-pressure results from various geological actions during the stage of petroleum generation, migration and accumulation in the basin.
出处
《石油实验地质》
CAS
CSCD
北大核心
1992年第3期296-301,共6页
Petroleum Geology & Experiment
