在克拉玛依地区沿克乌断裂带二十多年来曾完成多口钻井,反复进行过勘探及地质研究工作。早在五十年代末就已经确定了克乌断裂带的大致位置,并且根据钻井和局部地区的光点地震资料,认识到克乌断裂带为一组高角度逆断裂组成的“断阶带”,断面西北倾,倾角一般为60°—70°,并以此倾角向深部延伸,这是多年来对克乌断阶带的传统认识。 In Karamay area along the Kewu fault zone over 20 years have completed multiple drilling, repeated exploration and geological research. As early as the late 1950s, the approximate location of the Kewu fault zone has been determined. Based on the spot seismic data of drilling and local areas, it is recognized that the Kewu fault zone is a series of “fault zone belts” composed of high-angle reverse faults. , The northwest section of the section, the dip angle is generally 60 ° -70 °, and extending to the deep dip angle, which is the traditional understanding of Keru fault-step belt over the years.