摘要
共和地震的发震构造是人们普遍关注的重要问题。通过对共和地震的地质构造背景分析和地表断裂形变特征对比，确定共和地震的发震断裂为柴北缘断裂带，并对该断裂带的形成和发震、深部地球物理场特征做了深入的研究和探讨。
Seismic structure of Gonghe earthquake is an important problem.The authors have analyzed the geological tectonic background in Gonghe area,compared the surface fault deformation characteristics,determined that the seismic fault of Gonghe earthquake is in Caidamu northern fault,and discussed the form、development and deeply geophysical field characteristics.
出处
《高原地震》
1998年第4期11-17,共7页
Plateau Earthquake Research
关键词
发震演化及活动特征
共和地震
柴北缘断裂带
Developed evolution and active characteristic Gonghe earthquake Caidamu northern fault zone
