SEISMOLOGY AND GEOLOGY ›› 1989, Vol. 11 ›› Issue (2): 19-25.
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Zhao Gen-mu1, Wang Ruo-bai2, Liu Yu-tian2, Zhen Wen-jun1
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赵根模1, 王若柏2, 刘雨田2, 郑文俊1
基金资助:
Abstract: The traces and tectonic deformations of palaeoearthquake event hurried in Holocene strata in Beijing-Tianjin-Tangshan area have been studied in this paper. The study of Holocene strata and palaeo-environment suggests that the event occurred in the time when Holocene transgression ended in North China and coincided with a legend of disaster in ancient time 4000 years ago. Some phenomena related to this palaeo-earthquake have been discussed in this paper,such as seismic tectonic background, liquifaction of sandy basic in the strata, epicentre and magnitude of this event.
Key words: Beijing-Tianjin-Tangshan Area, Paleaoearthquake, Tectonic deformation
摘要: 本文介绍了京津唐地区内埋藏在全新世地层中的一次古地震遗迹和构造变形。通过对本区全新世地层、古环境的研究确定这次地震事件为距今4000年、本区海侵结束时发生的,恰恰与史料纪载的“地震传说”一致。文章最后对发震背景,砂基液化以及震中、震级等问题进行了一些讨论。
关键词: 京津唐地区, 古地震, 构造变形
Zhao Gen-mu, Wang Ruo-bai, Liu Yu-tian, Zhen Wen-jun. A STRONG EARTHQUAKE EVENT OCCURRED IN ANCIENT TIME IN BEIJING-TIANJIN-TANGSHAN AREA[J]. SEISMOLOGY AND GEOLOGY, 1989, 11(2): 19-25.
赵根模, 王若柏, 刘雨田, 郑文俊. 远古时代京津唐地区一次大震的研究[J]. 地震地质, 1989, 11(2): 19-25.
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