福建定点和流动跨断层对台湾强震的反映及特征研究  

Study on Responses of Fujian Stationary and Mobile Cross-Fault Deformations to Strong Earthquakes in Taiwan

作　　者：钟继茂[1] 李祖宁[1] 吴绍祖 陈光[1] 

机构地区：[1]福建省地震局,福建福州350003

出　　处：《华南地震》2008年第3期63-70,共8页South China Journal of Seismology

摘　　要：借助Matlab平台,应用能给出不同尺度下信号分解的近似部分和细节部分的小波变换方法,分析了福建省定点和流动跨断层场地的短水准形变观测资料。福建天马定点跨断层2003～2007年短水准观测资料的小波分析结果显示,分解到第七层的近似信号在极值和拐点出现前后往往有中强地震发生。由于福建省流动跨断层短水准测量为不定期观测,为取得等时间间隔的时序数据,我们采用三阶样条插值,在此基础上进行小波分析,发现分解到第三层的细节信号在台湾1999年"9.21"南投MS7.6级地震前有明显的年变规律被破坏的现象。With the help of Matlab platform, short leveling deformation observation data of stationary and mobile cross-fault sites in Fujian Province are analyzed by using the wavelet transform method, which is able to provide approximations and details of signal when it is decomposed at different scale levels. The results drawn from observation data of stationary cross- faults at Tianma from 2003 to 2007 show that moderate-strong earthquakes will probably occur before or after extreme values or knee points of the seventh level approximate decomposing signal appear. Because measurements of mobile cross-faults in Fujian are made at irregular the third-order spline interpolation method was applied to obtain time sequence data intervals, at equal intervals and then wavelet analyses were conducted. It is found that the yearly-changing pattern of the third detailed decomposed signal was disturbed before the Ms7.6 earthquake on Sept. 21, 1999 in Nantou, Taiwan.

关 键 词：短水准测量 小波分析 跨断层形变资料 样条插值 

分 类 号：P315.726[天文地球—地震学] U173.9[天文地球—固体地球物理学]