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东营凹陷沙三段、沙四段震积岩研究
引用本文:付文利,王艳琴,杨光,陈攀峰,郑胜利. 东营凹陷沙三段、沙四段震积岩研究[J]. 油气地质与采收率, 2004, 11(2): 6-8
作者姓名:付文利  王艳琴  杨光  陈攀峰  郑胜利
作者单位:1. 石油大学·东营
2. 胜利油田有限公司地质科学研究院
摘    要:根据地震作用过程,阐述了震积岩在岩心中的识别标志,建立了东营凹陷沙三段、沙四段碎屑震积岩的标准序列。分析结果表明,东营凹陷沙三段、沙四段沉积时期地震活动强烈且具周期性,并波及范围广。研究发现地震对地层的改造作用能改善砂岩储层的储集物性。

关 键 词:震积岩 岩心 储层 周期性 地层 砂泥液化现象 碳酸盐岩 震裂岩 孔隙度 渗透率
文章编号:1009-9603(2004)02-0006-03
修稿时间:2003-07-30

Study on seismite of Sha3 and Sha4 member in Dongying sag
Wenli,Wang Yanqin,Yang Guang. Study on seismite of Sha3 and Sha4 member in Dongying sag[J]. Petroleum Geology and Recovery Efficiency, 2004, 11(2): 6-8
Authors: Wenli  Wang Yanqin  Yang Guang
Abstract:cognition marks of the seismite in cores are analyzed and the clastic seismite standard sequence system in Sha3 and Sha4 member ( Es3, Es4 ) of Dongying sag is established based on the seismic action process. The analytic results present that the seismic movement was violent and has periodicity during the depositional stage of Es3 and Es4 in Dongying sag, and its sweep range is wide. It is found that seism process can improve sandstone reservoir quality.
Keywords:ismite   core   recognition mark   standard sequence   reservoir quality
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