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通过对塔里木盆地晚第三纪—第四纪沉积环境、沉积中心分布特征、构造变形特征及其动力学成因的分析，认为塔里木盆地晚第三纪—第四纪的沉积和构造变形过程明显受控于阿合奇—西昆仑—阿尔金左行剪切挤压构造。它加速了生油岩的成熟过程，形成新的背斜和断层圈闭构造，而且还控制了新生代油气的运移和聚集。非构造圈闭和断层遮挡圈闭所形成的次生油气藏是巴楚断隆的有利勘探目标。
Based on the analysis of sedimentary environment, distribution characteristics of sedimentary center, tectonic deformation and its dynamics in the Late Triassic to Quaternary in the Tarim Basin, it is concluded that the sedimentary and tectonic deformation processes of the Late Tertiary to Quaternary in the Tarim Basin are obviously affected by Controlled in the left part of the Achic-West Kunlun-Alking shear compression structure. It accelerates the maturation of source rocks, forms new anticlines and fault traps, and controls the migration and accumulation of Cenozoic hydrocarbons. Secondary reservoirs formed by non-structural traps and fault occlusion traps are favorable targets for the Bachu fault closure.