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安徽地区震源参数特征研究

STUDY ON CHARACTERISTICS OF SOURCE PARAMETERS IN ANHUI

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根据安徽数字测震台网记录的23个地震波形事件,首先采用Atkinson方法得到安徽地区的非弹性衰减特征,再用Moya方法得到24个台站的场地响应.在此基础上,扣除传播路径、场地响应和仪器响应的影响,利用遗传算法得到2009年以来安徽测震台网记录的42个ML≥2.0地震的震源参数,并对这些震源参数特征进行了系统的分析与研究.研究结果表明,安徽地区地震的地震矩与近震震级之间存在较好的线性关系,近震震级与矩震级存在一定的偏差,应力降与近震震级存在明显的正相关,震级越大,拐角频率越小,震源破裂半径越大.
According to 23 seismic waveforms recorded by Anhui digital earthquake network , they got inelastic attenuation through Atkinson method and site response from 24 stations through Moya method. Removing effect of propagation path 、 site response and instrument response, they got 42 source parameters of earthquakes with ML≥2.0 recorded by Anhui earthquake network since 2009 using genetic algorithms method and made a systematic analysis on characteristics of it. The results show that: there is a good linear relationship between earthquake moment and local magnitude in Anhui ; there is a certain bias between the local magnitude and moment magnitude; there is a clear positive correlation between stress drop and local magnitude; the larger the magnitude is , the smaller the corner frequency is and the greater the radius of rupture is.

Source parametersNon-elasticity attenuationSite responseEarthquake momentStress drop

戚浩、夏仕安、张炳、程鑫、王琐琛

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安徽省地震局,安徽合肥230031

震源参数 非弹性衰减 场地响应 地震矩 应力降

地震科技星火计划安徽省地震局重点科研基金大别山实验场资助

XH1202420110501

2012

内陆地震
新疆维吾尔自治区地震局

内陆地震

CSTPCD
影响因子:0.495
ISSN:1001-8956
年,卷(期):2012.26(3)
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