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准噶尔盆地西北缘走滑断层特征及油气地质意义
Characteristics of Strike-Slip Faults in the Northwestern Margin of Junggar Basin and Their Geological Significance for Petroleum
【摘要】 准噶尔盆地西北缘前陆冲断带构造样式复杂多样,除规模较大的逆断层外,还发育一系列北西向的走滑断层。以高分辨率三维地震资料为基础,对断裂体系分析表明克拉玛依—百口泉地区的走滑断层可分为花状走滑断层和简单走滑断层两类,二者在成因、剖面特征等方面具有明显差别。研究结果认为走滑断层对油气的运聚成藏具有重要的双重控制作用,即能作为有效的运移通道,又能够起遮挡作用而形成圈闭。
【Abstract】 The foreland thrust belt has complex and various structural styles.Besides the large-scale reverse faults,there are a series of north-west strike-slip faults.Based on high-resolution seismic data,the foreland fault systems in the NW margin of Junggar basin were analyzed.It reveals that the strike-slip fault system of Ke-Bai area can be divided into two types,namely the flower strike-slip faults and the simple strike-slip faults,which have obvious differences in genesis and section features. The strike-slip faults have dual influence on hydrocarbon migration and accumulation.They can not only be effective migration channels for petroleum,but also can seal petroleum.
【Key words】 foreland thrust belt; strike-slip faults; flower structure; Junggar basin;
- 【文献出处】 高校地质学报 ,Geological Journal of China Universities , 编辑部邮箱 ,2008年02期
- 【分类号】P618.130.2
- 【被引频次】21
- 【下载频次】773