卡因迪克背斜位于准噶尔盆地南缘，乌苏市北西约20 km处，构造区划上属准噶尔盆地北天山山前坳陷四棵凹陷，位于凹陷边缘向车排子隆起逐渐抬升的过渡带。近日完钻的卡6井在白垩系和下第三系获得工业油流。 卡因迪克背斜以西发育两个低幅度背斜圈闭，由西向东为卡西2号背斜、卡? The Cavendish anticline is located at the southern margin of Junggar Basin and about 20 km northwest of Wusu. The structural division belongs to the Sinka depression in the northern part of the northern Tianshan Mountain in the Junggar Basin, and is located at the transitional zone where the uplift of Chepaizi rises gradually along the edge of the depression. Recently, the Well Drilling 6 well received industrial oil flow in the Cretaceous and Lower Tertiary. Two low amplitude anticlinal traps developed west of the Cainedi anticline, from west to east to the Kasia anticline 2,