SEISMOLOGY AND GEOLOGY ›› 1981, Vol. 3 ›› Issue (2): 57-64.
• Brief Report • Previous Articles Next Articles
Peng Yimin1, Li Dingrong2, Xie Zhenzhao2, Wang Ande2, Liu Qingsi3
Received:
Online:
Published:
彭一民1, 李鼎容2, 谢振钊2, 王安德2, 刘清泗3
Abstract: By the data obtained- from the seismogeological work in the Beijing plain, the authors supposed that all the main active faults in this region were of contemporaneous nature and originated at the same time as the deposition took place. In our opinion, the study of contemporaneous faults is of great significance. At the end of this paper a general morphological model for contemporaneous faults is presented.
摘要： 本文通过在北京平原区进行地震地质工作所获得的实际资料,提出本区主要活动断裂均属在沉积建造形成的同时所生成的同生断裂,并对研究同生断裂的意义提出了初步看法,最后总结了同生断裂的一般形态模式。
Peng Yimin, Li Dingrong, Xie Zhenzhao, Wang Ande, Liu Qingsi. SOME FEATURES OF CONTEMPORANEOUS FAULTS IN BEIJING PLAIN AND THEIR SIGNIFICANCE[J]. SEISMOLOGY AND GEOLOGY, 1981, 3(2): 57-64.
彭一民, 李鼎容, 谢振钊, 王安德, 刘清泗. 北京平原区同生断裂的某些特征及其研究意义[J]. 地震地质, 1981, 3(2): 57-64.
0 / / Recommend
Add to citation manager EndNote|Ris|BibTeX
URL: https://www.dzdz.ac.cn/EN/
https://www.dzdz.ac.cn/EN/Y1981/V3/I2/57
