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Intracontinental basins and strong earthquakes
作者姓名:邓起东  高孟潭  赵新平  吴建春
作者单位:Institute of Geology,China Earthquake Administration,Beijing 100029,China,Institute of Geophysics,China Earthquake Administration,Beijing 100081,China,Earthquake Administration of Shanxi Province,Taiyuan 030002,China,China Earthquake Administration,Beijing 100036,China
摘    要:Introduction A M=8 earthquake occurred in the intracontinental Linfen basin on September 17, 1303. This is the Hongtong M=8 earthquake in Shanxi Province. It is the first recorded M = 8 earthquake since the Chinese historical seismic records had started. The earthquake killed 200 000 people (LI, 1960; XIE, CAI, 1983). The year 2003 is the 700th anniversary of the earthquake occurrence. In memory of the people died in the earthquake, for further improving earthquake prevention and disas…

收稿时间:9 December 2003
修稿时间:12 March 2004

Intracontinental basins and strong earthquakes
Deng Qi-dong , Gao Meng-tan , Zhao Xin-ping and Wu Jian-chun.Intracontinental basins and strong earthquakes[J].Acta Seismologica Sinica(English Edition),2004,17(4):377-380.
Authors:Deng Qi-dong  Gao Meng-tan  Zhao Xin-ping and Wu Jian-chun
Institution:1. Institute of Geology, China Earthquake Administration, Beijing 100029, China
2. Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
3. Earthquake Administration of Shanxi Province, Taiyuan 030002, China
4. China Earthquake Administration, Beijing 100036, China
Abstract:The September 17, 1303 Hongtong M=8 earthquake occurred in Linfen basin of Shanxi down-faulted basin zone. It is the first recorded M=8 earthquake since the Chinese historical seismic records had started and is a great earth-quake occurring in the active intracontinental basin. We had held a Meeting of the 700th Anniversary of the 1303 Hongtong M=8 Earthquake in Shanxi and a Symposium on Intracontinental Basins and Strong Earthquakes in Taiyuan City of Shanxi Province on September 17~18, 2003. The articles presented on the symposium discussed the relationships between active intracontinental basins of different properties, developed in different regions, in-cluding tensional graben and semi-graben basins in tensile tectonic regions, compression-depression basins and foreland basins in compressive tectonic regions and pull-apart basins in strike-slip tectonic zones, and strong earth-quakes in China. In this article we make a brief summary of some problems. The articles published in this special issue are a part of the articles presented on the symposium.
Keywords:the Hongtong M=8 earthquake  Shanxi  intracontinental basin  strong earthquake
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