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在塔里木地台北缘库鲁克塔格断隆上,发现晚元古宙帕尔岗群与其下伏兴地塔格群之间为角度不整合。进一步研究了中元古宙兴地塔格群和晚元古宙帕尔岗塔格群在沉积建造、变质作用、构造样式和岩浆活动等方面的差异,证明中元古宙末期曾发生强烈构造运动——兴地运动。它在1.3～1.4Ga达到高潮,0.95～1Ga时结束,形成塔里木地台基底。根据构造要素的叠加关系和变形特征,将这次构造运动划分为三个变形幕。
On the Kuruktag fault break on the northern margin of the Tarim Platform, it was found that the Palaeozoic Paleo-Proterozoic group is not angularly integrated with its underlying Hindgartag group. Furthermore, the differences of sedimentary structures, metamorphism, tectonic styles and magmatism between the Xingtaitag Group of the Proterozoic and the Paleangagroup of the Late Proterozoic were further studied. It was proved that strong structures occurred in the late Proterozoic Exercise - Hing to exercise. It reached the climax of 1.3 ~ 1.4Ga, 0.95 ~ 1Ga when the end of the formation of Tarim platform basement. According to the superposition relations and deformation features of the structural elements, this tectonic movement is divided into three deformation curtains.