车莫古隆起为燕山期形成的横跨准噶尔盆地的大型古隆起,通过利用地震剖面“层拉平”的手段将车莫古隆起的发育演化划分为初始形成阶段(J1)、强烈发育阶段(J2+3)、隐伏埋藏阶段(K—E)和掀斜消亡阶段(N—Q)4个阶段,在此基础上分析了车莫古隆起对腹部地区油气成藏的影响。车莫古隆起的发育和演化为盆地腹部地区创造了独特的油气运聚背景和圈闭条件,决定了腹部探区具有多期构造演化与多期成藏的特点。 The Mogul uplift is a large paleo-uplift that straddles the Junggar Basin during the Yanshanian Period. The development and evolution of the Che Mogu uplift are divided into initial formation stage (J1) and intensive development stage (J2) by using the “stratification leveling” +3), K-E and N-Q phases. Based on this, the influence of Chemo-Mo uplift on hydrocarbon accumulation in the belly region was analyzed. The development and evolution of the Moogu uplift created unique hydrocarbon accumulation and trapping conditions for the belly of the basin and determined the characteristics of multi-phase tectonic evolution and multi-phase accumulation in the belly exploration area.