新疆西准噶尔华力西地槽褶皱带地质构造的展布,与其相邻两侧的天山和阿尔泰地区迥然不同。据新近科研成果,已查实西准噶尔西南部存在着一系列的弧形构造带(图1)。其中以拉巴—达拉布特弧形断裂带最具代表性,不但规模大,地表暴露的清晰完整,而且研究的亦较详细。现整理成文,供参考指正。 The distribution of the geotectonic structure of the Glimpse Fold Belt in the West Lhasa, West Junggar, Xinjiang is very different from the adjacent Tianshan and Altai areas. According to recent scientific research, it has been verified that a series of arc structural zones exist in the southwestern part of West Junggar (Figure 1). Among them, the Laba-Dalbot arcuate fault zone is the most representative, which not only has a large scale but also has a clear and complete surface exposure. In addition, the study is also more detailed. Now finishing documents for reference correction.