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SITE EFFECT ASSESSMENT OF SEISMOLOGICAL STATIONS OF ALBANIA THROUGH HVNR TECHNIQUE

机译:HVNR技术对阿尔巴尼亚地震台站的现场效果评估

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In this paper is presented the study of site response parameters of Albanian Seismological Stations (ASN) from ambient noise measurements and felt earthquakes. The seismological stations of Albania which use the VSAT communication technology are located generally in hard rock formations. The aim of Methodology is to compare the response parameters of the sites (fundamental frequency, amplification) for registered seismic signals, from microtremors and the earthquakes as well. The predominant frequency of the site of every seismological station site is determined using the methodology of Horizontal to Vertical Spectral Ratio (HVNR), of the triggered noise and several felt earthquakes in Albania territory. From the results of this study, is concluded that fundamental frequency (F_0) and the amplification in this frequency (A_0), are almost the same for the microtremors and seismic events. As far as for the amplification factor, we concluded that on the sites of seismological stations situated on hard rock (basement) there is not amplification. In the contrary, for the Vlora station site, the amplification factor is 5-6 at fundamental frequency 6 Hz, showing that this station is not situated on the hard rock. The microtremors are a useful technique for the site assessment effects, used in microzonation of urban areas, that complement the lack of seismic data in a region (boreholes, geology, etc.)
机译:本文介绍了从环境噪声测量和毛毡地震对阿尔巴尼亚地震台站(ASN)的场地响应参数的研究。使用VSAT通信技术的阿尔巴尼亚地震台站通常位于硬岩层中。方法学的目的是比较微震和地震中记录的地震信号的站点响应参数(基本频率,放大率)。每个地震台站的主要频率是使用水平与垂直光谱比(HVNR),触发噪声和阿尔巴尼亚境内几次毡状地震的方法确定的。从这项研究的结果可以得出结论,对于微震和地震事件,基本频率(F_0)和在该频率上的放大倍数(A_0)几乎相同。关于放大系数,我们得出结论,在位于硬岩(基底)上的地震台站上没有放大。相反,对于Vlora站站点,在6 Hz的基频处,放大系数为5-6,这表明该站不位于硬岩上。微震是一种用于现场评估效果的有用技术,用于城市区域的微区划,弥补了该地区缺乏地震数据(钻孔,地质等)的不足。

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