【摘要】 东秋里塔格构造带发育的新近系吉迪克组膏盐层,在库车组沉积时期以来的构造变形过程中起到了滑脱和调节地层变形的作用,地震剖面解释结果表明,盐上构造圈闭主要有盐上背斜、盐上逆冲断层遮挡圈闭等;盐层内部圈闭是由其中碳酸盐岩和砂岩夹层所形成的岩性和褶皱圈闭;盐下构造圈闭主要有盐下背冲断块圈闭等。结合研究区的成藏条件认为研究区具有以断裂和不整合为输导层的它源-侧向排烃油气成藏模式,主要构造活动期与阳霞凹陷的烃源岩演化有着很好的匹配关系,使研究区构造圈闭内聚集了大量来自阳霞凹陷的天然气。更多还原

【Abstract】 The thick Neogene salt layer developed in the Eastern part of Qiulitage Belt, through the representative seismic profiles, it is reveled that the salt layer is a decollement layer and adjustes the differentiated deformation between the supra-salt layer and the sub-salt layers, the structural traps in the supra-salt layer are mainly anticline trap, thrust fault sheltering trap, etc, the traps in the salt layer are mainly the lithostratigraphic trap or the anticline trap constituted of the carbonate rock and the sandstone, the structural traps in the sub-salt layer are mainly the pop-up etc. Combining this result with analyzing of the condition of the hydrocarbon accumulation, the authors consider there is the accumulation pattern of separated source-side rejecting in the area with a transporting layer composed of faults and unconformities, there is a good relationship between the evolution history of the source rock in Yangxia Sag and the structural deformation, all these make the structural traps in the studied area capture the natural gas generated in Yangxia Sag.更多还原