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Site Response for the RSM Seismic Network and Source Parameters in the Central Apennines (Italy)

机译:亚平宁中部(意大利)RSM地震台网的现场响应和震源参数

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— Thirty-three earthquakes which occurred in the Central Apennines (Italy) with Ml ranging from 2.4 to 3.7 have been spectrally analysed using digital recordings from twelve stations of the Rete Sismometrica Marchigiana (RSM) network. Data corrected for geometrical spreading and quality factor Q have been inverted by means of the Generalised Inversion Technique. Site responses have been compared with those obtained by H/V ratio. Site amplifications have been observed both at stations placed on Pleistocene sediments and at one station located at 1800 m altitude. Source parameters have been calculated by fitting the spectra with an automatic procedure adopting the ω2 source model. The seismic moments range from 9.23 × 1019 to 4.28 × 1021 dyne-cm with an average M 0 (S) to M 0 (P) ratio of 1.13 ± 0.38. The stress drops are generally low and they vary between 1.1 and 10.2 bar when estimated by using S source spectra, and between 0.5 and 7.1 bar when the P-source spectra are fitted. For the considered range of seismic moments we observe that the stress drop does not have significant dependence on event size.
机译:—使用来自Rest Sismometrica Marchigiana(RSM)网络的十二个站的数字记录,对在中亚平宁山脉(意大利)发生的33震级为2.4至3.7的地震进行了频谱分析。已通过广义反演技术反演校正了几何扩展和品质因数Q的数据。站点响应已与通过H / V比获得的站点响应进行了比较。在位于更新世沉积物的台站和海拔1800 m的一个台站都观察到了站台放大。源参数是通过采用ω2源模型的自动程序对光谱进行拟合来计算的。地震矩范围从9.23×1019 到4.28×1021 达因-厘米,平均M 0 (S)与M 0 (P)之比为1.13±0.38 。应力降通常较低,使用S源光谱估算时,应力降在1.1至10.2 bar之间,而拟合P源光谱时,应力降在0.5至7.1 bar之间。对于考虑的地震矩范围,我们观察到应力降与事件大小没有显着相关性。

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