安宁河断裂带位于四川省西南部,是我国西南地区一条规模较大的、具有长期发育历史的深大断裂带。新第三纪以来,该断裂带新构造运动强烈。我们根据在西南地区进行地震地质考察取得的有关资料,并结合前人研究成果,对安宁河断裂带新构造运动的迹象、类型及特征作了初步综合分析,得出几点粗浅的看法,草成此文提出来与大家共同讨论。 The Anninghe fault zone is located in the southwestern Sichuan Province and is a large-scale deep-fault zone with long-term development history in southwest China. Since the Neogene, the new tectonic movement of the fault zone was strong. Based on the relevant data obtained from the seismological and geological survey in southwest China and based on the previous research results, we make a preliminary and comprehensive analysis of the signs, types and characteristics of the Neotectonic movement in the Anninghe fault zone and draw some superficial opinions. This article is put forward to discuss with you.