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为了研究强震发生带构造背景的规律性,必须用统一的观点比较不同地区的资料。以南斯拉夫迪纳拉山和苏联科彼特山为例进行对比。两个褶皱系均位于阿尔卑斯褶皱带内,并在构造和发育史方面都有许多相似特点:如最大主地槽和造山建造有相似的组分和相近的年代,褶皱和许多断裂的形态相似,主要构造带相对位置一致,并有类似的发育史。亚得利亚海沿岸切尔诺哥利亚(南斯拉夫)和苏联南土库曼阿什哈巴德地区是这一褶皱系内相
In order to study the regularity of tectonic setting of strong earthquake occurrence zones, we must compare the data of different regions with a unified view. Taking Yugoslavia’s Mount Dinara and Soviet Kopit Hills as examples. Both fold systems are located within the Alps fold belt and share many similarities in tectonic and developmental history: the crests and many fractures have similar morphologies similar to the largest component of the main trough and the orogenic structures and their similar age, The main tectonic belts have the same relative position and similar developmental history. The Chernobyl-Yugoslavia (Yugoslavia) coast of the Adriatic Sea and the southern Turkmenistan Ashgabat region of the Soviet Union are the inner parts of this fold system