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1679年三河-平谷8级地震发震断层的古地震及其重复间隔

PALEOEARTHQUAKES AND RECURRENCE INTERVAL ON THE SEISMOGENIC FAULT OF 1679 SANHE PINGGU M 8 EARTHQUAKE, HEBEI AND BEIJING

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【作者】 冉勇康邓起东杨晓平张晚霞李如成向宏发

【Author】 Ran Yongkang Deng Qidong Yang Xiaoping Zhang Wanxia Li Rucheng Xiang Hongfa (Institute of Geology, SSB, Beijing 100029)

【机构】 国家地震局地质研究所

【摘要】 通过大探槽开挖和断层陡坎分析,揭示出发生于1679年8级地震的新夏垫断层自距今约2万a以来共发生了4次地震事件。前两次为砂体液化显示的事件;后两次为可见直接断错证据的事件。分析得到的1679年地震最大垂直位移为1.75m,前1679年事件为1.41m,是两次震级非常接近的特征地震。4次事件发生的时间分别为距今约20000,13000,7500和317a,平均重复间隔时间为(6561±691)a,显示了准周期重复的特征。

【Abstract】 The 4 paleoearthquake events that have occurred on seismogenic fault of 1679 Sanhe Pinggu M 8 Earthquake since 20ka B.P. are exposed through the analysis of trenches and fault scarp profiles. The earlier two events are marked by liquefaction and the later two events are shown by direct fault offset, including the 1679 event. The 1679 event and pre 1679 event are two characteristic earthquakes of which the maximum displacement is about 1.75m and 1.41m, respectively and the intensity of two events is very close. The occurrence time of 4 events was about 20 000, 13 000, 7 500 and 317a B.P., respectively. Average interval of recurrence is (6 561±691)a. It indicates the characteristics of quasi periodic occurrence of earthquakes.

  • 【文献出处】 地震地质 ,SEISMOLOGY AND GEOLOGY , 编辑部邮箱 ,1997年03期
  • 【分类号】P315.1
  • 【被引频次】98
  • 【下载频次】439
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