翟洪涛, 刘欣, 刘庆忠, 张毅. 江淮地区地震烈度衰减关系的研究[J]. 华北地震科学, 2003, 21(4): 30-34.
引用本文: 翟洪涛, 刘欣, 刘庆忠, 张毅. 江淮地区地震烈度衰减关系的研究[J]. 华北地震科学, 2003, 21(4): 30-34.
ZHAI Hong tao, LIU Xin, LIU Qing zhong, ZHANG Yi. STUDY ON THE ATTENUATION OF SEISMIC INTENSITY IN JIANGHUAI AREA[J]. North China Earthquake Sciences, 2003, 21(4): 30-34.
Citation: ZHAI Hong tao, LIU Xin, LIU Qing zhong, ZHANG Yi. STUDY ON THE ATTENUATION OF SEISMIC INTENSITY IN JIANGHUAI AREA[J]. North China Earthquake Sciences, 2003, 21(4): 30-34.

江淮地区地震烈度衰减关系的研究

STUDY ON THE ATTENUATION OF SEISMIC INTENSITY IN JIANGHUAI AREA

  • 摘要: 地震烈度衰减关系具有较强的地区性,这是由于不同地区的震源特性、传播介质和场地条件的不同而引起。研究区(北纬29°~35°,东经114°~120°)位于华北地震区和华南地震区之间的过渡地区,地震活动性总体水平不高,烈度衰减关系有其自身的震源特性、传播介质和场地衰减特性等。本次工作重新挑选震例,对研究区的地震烈度衰减规律进行了统计回归分析,并与该地区已有的地震烈度衰减关系进行认真的比较分析。

     

    Abstract: Since the difference of focal character, media and site, attenuation of earthquake intensity is different in regions. The seismicity of the studying area (29°~35°N, 114°~120°E), which is located in the transition area of earthquake region in North China and South China, is not high, and the attenuation of intensity has its own characters in focal mechanism, radiate medium and site. The attenuation of intensity in the area was analyzed with statistical regression, and compared with existing results.

     

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