| 重庆及邻近地区水平向基岩地震动加速度峰值与反应谱衰减关系 |
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| 引用本文： | 蔡辉腾,李英民,郑清,郑师春.重庆及邻近地区水平向基岩地震动加速度峰值与反应谱衰减关系[J].四川地震,2007(2):11-15. |
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| 作者姓名： | 蔡辉腾 李英民 郑清 郑师春 |
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| 作者单位： | 1. 福建省地震局,福建福州,350003
2. 重庆大学 土木工程学院,重庆,400045 |
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| 摘 要： | 结合重庆及邻近地区地震烈度衰减关系,选择有丰富强震记录和地震烈度资料的美国西部作为参考地区,采用转换方法,得到重庆及邻近地区基岩水平地震动加速度峰值与反应谱衰减关系。
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| 关 键 词： | 地震动 衰减关系 重庆及邻近地区 |
| 文章编号： | 1001-8115（2007）02-0011-05 |
| 修稿时间： | 2007-01-042007-04-06 |
Attenuation relations for acceleration peak and response spectrum of horizontal earthquake motions in Chongqing and its adjacent region |
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| CAI Hui-teng,LI Ying-min,ZHENG Qing,ZHENG Shi-chun.Attenuation relations for acceleration peak and response spectrum of horizontal earthquake motions in Chongqing and its adjacent region[J].Earthquake Research in Sichuan,2007(2):11-15. |
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| Authors: | CAI Hui-teng LI Ying-min ZHENG Qing ZHENG Shi-chun |
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| Institution: | 1 Earthquake Administration of Fujian Province, Fujian Fuzhou 350003, China; 2 College of Civil Engineering, Chongqing University, Chongqing 400045, China |
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| Abstract: | Based on the seismic intensity data of Chongqing and its adjacent region,the attenuation relation of seismicity intensity is determined.Since the western America has rich strong motion records and seismic intensity data,we select these data as the references and use the means of conversing method in Chongqing and its adjacent regions to obtain the attenuation relations for acceleration peak and response spectrum of matrix horizontal earthquake motions. |
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| Keywords: | earthquake motion attenuation relations Chongqing and its adjacent region |
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