The Karamaili faulting belt is well-known in the Northern Xinjiang and Central Asian area, and it came into being after the closure of the Paleozoic ocean.
卡拉麦里断裂带是新疆北部乃至中亚地区一条显著的大型断裂带，是在古生代洋盆关闭以后形成的。
Since the Cenozoic the neotectonic movement in the Western area of Beijing has been dominated by non-isostatic vertical differential uplifting, with many faulting, tilting and horizontal mov…
新生代以来，西山区新构造运动以不均衡的垂向差异性上升运动为主，兼有掀斜运动、断裂运动和水平运动。
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