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地质、地震和重磁力资料综合研究表明,乌鲁木齐—米泉断裂是一条呈NE向延伸的大型左行压扭走滑基底断裂,地表浅层表现为以左行压扭走滑变形组合为主的大型复杂构造变形带,平面上切割并错断NWW向和近EW向断裂。该断裂经历了印支末期、燕山期和喜马拉雅期多期构造活动,对其两侧地区的构造演化和油气成藏条件具有重要影响。沿断裂带形成的一系列呈雁行排列的大型背斜、斜坡带和隆起是油气聚集的有利地区。
The comprehensive study of geology, earthquakes and gravity and magnetic data shows that the Urumqi-Miquan fault is a large left-lateral compressive and torsional strike-slip fault ruptured in NE direction, and the surface superficial is characterized by a large-scale Complex structural deformation zone, the plane cutting and the wrong NWW and near EW fracture. The fault experienced multi-stage tectonic activities during the Indosinian, Yanshanian and Himalayan periods and has an important influence on tectonic evolution and hydrocarbon accumulation conditions on both sides of the fault. A series of large anticlines, ramp zones and uplift formed along the fault zone are geotectonic favorable areas.