西南石油大学学报（自然科学版）2011，Vol.33Issue(6)：55-59,5.DOI:10.3863/j.issn.1674-5086.2011.06.010
大邑地区须家河组储层裂缝特征及主控因素
范存辉 1秦启荣 1赵玲 2钟灵3
作者信息
- 1. 西南石油大学资源与环境学院,四川成都610500
- 2. 中国石化西南油气分公司工程监督中心,四川德阳618000
- 3. 中国石化中原石油勘探局钻井工程技术研究院,河南濮阳457001
- 折叠
摘要
Abstract
The reservoirs of Xujiahe Formation in Dayi area are super tight sandstone reservoir, and the reservoir petrophysical property is poor. The existence of fractures greatly improves the reservoir permeator. There are tectonic fractures, diagenetic fractures and abnormal high-pressure fractures in this area. There exists drilling induced fractures in some wells. Tectonic fractures develop well among them, which is the key types of factures. The tectonic fractures of this area mainly take the form of low-angle and high-angle fractures. The distribution of fractures development is controlled obviously by faults. Fracture-developed zone presents zebraic distribution along east-north fault belt, where faults clip zone as well as the fracture in high-steep part of structure develop better. The controlling factors of the fractures development mainly include tectonic stress, tectonic position, rock types, rock stratum, etc. The tectonic position and rock types are the key factors controlling the development and distribution of the fractures.关键词
储层分析/须家河组/裂缝/构造缝/四川盆地Key words
reservoir analysis/ Xujiahe Formation/ fracture/ structural fractures/ Sichuan Basin分类
能源科技引用本文复制引用
范存辉,秦启荣,赵玲,钟灵..大邑地区须家河组储层裂缝特征及主控因素[J].西南石油大学学报（自然科学版）,2011,33(6):55-59,5.
