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鸟山构造带位于塔里木盆地西南坳陷与巴楚隆起的分界部位,和田河气田区的西缘,是塔里木盆地内部重要的构造单元。本次研究结合钻井、地震等第一手资料,将鸟山构造带重新划分为3个次级构造:鸟山主体构造、鸟山东构造、鸟山北构造,并通过不整合面、平衡剖面等资料划分出8个构造演化阶段。鸟山主体构造与玛扎塔格构造原属一体,因差异应力作用而在发育撕裂断层(鸟山东断裂)之后两者分离,全新世晚期受晚喜马拉雅运动影响在鸟山、玛扎塔格、古董山之间发育右行走滑的鸟山北断裂。该构造带具有良好的石油地质条件,鸟山东构造带是该区最有潜力的区块,同时鸟山主体构造带也是该区比较有潜力的勘探区块。
The Toriyama structural belt is located in the boundary between the southwestern depression and Bachu uplift in the Tarim Basin and the western margin of the Hetianhe gas field. It is an important tectonic unit in the interior of the Tarim Basin. Based on the first-hand data of drilling and earthquakes, this study re-divides the Toriyama structural belt into three secondary structures: the main structure of Toriyama, the structure of Toriyama and the North of Toriyama and passes the data of unconformity and balance Divided eight tectonic evolution stages. The main body structure of the Toriyama Mountain is one with Mazatag structure. After the development of the tearing fault (the Bird-Shankong fault), the two belts separate due to the differential stress. In the Late Holocene, , The development of ancient mountains right between the slippery bird north fault. The structural belt has good petroleum geological conditions. The Bird-Shandong tectonic belt is the most potential block in this area, and the main structure zone of Bird’s Rock is also a potential exploration block in this area.