利用成像测井资料研究车古201潜山裂缝发育控制因素  

Research of the factors controlling fracture development of Chegu 201 buried hill fracture by FMI

作　　者：宋胜浩[1] 

机构地区：[1]大庆石油学院电子科学学院,黑龙江大庆163318

出　　处：《大庆石油学院学报》2006年第1期18-20,共3页Journal of Daqing Petroleum Institute

基　　金：国家973项目(G1999043303)

摘　　要：利用地层微电阻率扫描成像测井资料,分析了车古201潜山裂缝的发育特征.结果表明:裂缝发育程度主要受岩性和断层、褶皱等构造因素的控制.其中岩性是影响裂缝发育程度的重要内在因素,构造因素是影响碳酸盐岩裂缝发育程度的重要外部条件.The development characteristic of the fractures of Chegu 201 buried hill are analyzed making use of the formation micro-scanner log data.The result shows that the development degree of fractures is mainly controlled by lithology and tectonic conditions especially faulting and folding.The lithology is the inner factor to influence the development of fractures and the tectonic condition improved the reservoir of carbonate rocks buried hill.

关 键 词：潜山 裂缝 微电阻率成像测井 控制因素 

分 类 号：P618.130[天文地球—矿床学]