LUO RONGLIAN, LIU ZHENGRONG, CHEN YURUcom sh advance. 1984: THE VARIATION OF SEISMICITY PATTERN IN NORTH CHINA. Acta Seismologica Sinica, 6(2): 129-134.
Citation: LUO RONGLIAN, LIU ZHENGRONG, CHEN YURUcom sh advance. 1984: THE VARIATION OF SEISMICITY PATTERN IN NORTH CHINA. Acta Seismologica Sinica, 6(2): 129-134.

THE VARIATION OF SEISMICITY PATTERN IN NORTH CHINA

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  • Published Date: August 31, 2011
  • By studying the temporal-spatial distribution of seismicity in North China (34-42N, 108-124 B) it clearly shows that the transfer of the main seismic activity for different areas within different periods is quite obvious. The rift belt in front of the Taihangshan Range is one of the most important tectonic zones in this region which controls not only'the seismicity of its two ends but also that of both to the east and west of the belt. It is pointed out that since about the 19th century, seismic activity was chiefly in the east. The seismicity pattern has been evidently varied. This fact may be important in monitoring areas of future occurrences of earthquakes. It is significant for long-term earthquake prediction.
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    [2] 河北省地震局分析预报室地履地质组(贾云年执笔),关于河北省地震危险性的探讨,地球物理学报,20, 3,232——241, 1977,

    [3] 杨理华,李钦祖,华北地区地壳应力场,地震出版社,1980.

    [4] 邓起东,范福田,华北断块区新生代、现代地质构造特征,华北断块区的形成与发展,192——205,科学出版社,1980,

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    [7] 国家地展局分析预报中心,中国东部地展月录,地震出版社,1980.

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    [9] 刘正荣,罗荣联,陈玉茹,川滇地震活动的格局及周期,地震研究,6, 1, 97——108, 1983.

    [1] 刘行松,纵贯中国东部一条新的巨型构造带,地震地质,1, 1, 29——38, 1979.

    [2] 河北省地震局分析预报室地履地质组(贾云年执笔),关于河北省地震危险性的探讨,地球物理学报,20, 3,232——241, 1977,

    [3] 杨理华,李钦祖,华北地区地壳应力场,地震出版社,1980.

    [4] 邓起东,范福田,华北断块区新生代、现代地质构造特征,华北断块区的形成与发展,192——205,科学出版社,1980,

    [5] 国家地震局,中国地震烈度区划工作报告,地震出版社,1981,

    [6] 国家地展局,中国强震简目,地震出版社,1977.

    [7] 国家地展局分析预报中心,中国东部地展月录,地震出版社,1980.

    [8] 李善邦,Г.П.果尔什可夫,中国地震区域划分图及其说明,地球物理学报,6, 2, 127——158, 1957.

    [9] 刘正荣,罗荣联,陈玉茹,川滇地震活动的格局及周期,地震研究,6, 1, 97——108, 1983.
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