早印支运动结束了吉林省北部地槽的发展进程,从而南台北槽统一为一体。早印支运动具有华力西构造运动的继承性,晚印文运动时期则具有中生代构造运动的新生性特点。北部地槽是递进式封闭的华力西地槽印支皱褶带。印支运动时期是在亚洲大陆与太平洋构造体系中首次出现大陆边缘活化带的新起点。 The early Indo-Chinese Movement ended the development of the geosyncline in the northern part of Jilin Province, and unified the Southern Taipei Slots. The Early Indosinian Movement has the inheritance of the Variscan tectonic movement and the late Indosinian Movement has the characteristics of Mesozoic tectonic movement. The northern trough is a progressive enclosed Variscan trough fold fold belt. The Indo-Chinese Movement is a new starting point for the first time in the Asian continental and Pacific tectonic systems that the continental margin activated zone appeared.