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Site effect assessment of seismological stations of Albania through HVNR technique cosmology

机译:通过HVNR技术宇宙学评价阿尔巴尼亚地震台地效应

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In this paper is presented the study of site response parameters of AlbanianSeismological Stations (ASN) from ambient noise measurements and felt earthquakes.Theseismological stations of Albania which use the VSAT communication technology are locatedgenerally in hard rock formations.The aim of Methodology is to compare the response parameters of the sites (fundamentalfrequency, 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 usingthe methodology of Horizontal to Vertical Spectral Ratio (HVNR), of the triggered noise and severalfelt earthquakes in Albania territory.From the results of this study, is concluded that fundamentalfrequency (F0) and the amplification in this frequency (A0), are almost the same for the microtremorsand seismic events.As far as for the amplification factor, we concluded that on the sites ofseismological stations situated on hard rock (basement) there is not amplification.In the contrary, forthe Vlora station site, the amplification factor is 5" at fundamental frequency 6 Hz, showing that thisstation is not situated on the hard rock.The microtremors are a useful technique for the siteassessment effects, used in microzonation of urban areas, that complement the lack of seismic data ina region (boreholes, geology, etc.
机译:本文通过环境噪声测量和毛毡地震研究了阿尔巴尼亚地震台站的现场响应参数。使用VSAT通信技术的阿尔巴尼亚地震台站一般位于硬岩层中,方法学的目的是比较来自微震和地震的已记录地震信号的位点的响应参数(基本频率,放大率)。每个地震台站位点的主要频率是使用水平和垂直频谱比(HVNR)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(F0)和该频率的放大倍数(A0)几乎相同。 ,我们得出结论,在位于硬地带的地震台站上ck(地下室)没有放大。相反,对于Vlora电台站点,在6 Hz的基频处放大因子为5“,这表明该电台不在硬岩上。微震是一种用于站点评估的有用技术用于城市区域微区化的效应,弥补了该地区缺乏地震数据(钻孔,地质等)的不足。

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