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Site Characterization of Italian Strong Motion Recording Stations

机译:意大利强运动录音站的现场特征

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A dataset of site conditions at 101 Italian ground motion stations with recorded motions has been compiled that includes geologic characteristics and seismic velocities. Geologic characterization is derived principally from local geologic investigations by ENEL that include detailed mapping and cross sections. For sites lacking such detailed geologic characterization, the geology maps of the by Servizio Geologico d'Italia are used. Seismic velocities are extracted from the literature and the files of consulting engineers, geologists and public agencies for 33 sites. Data sources utilized include post earthquake site investigations (Friuli and Irpinia events), microzonation studies, and miscellaneous investigations performed by researchers or consulting engineers/geologists. Additional seismic velocities are measured by the authors using the controlled source spectral analysis of surface waves (SASW) method for 18 sites that recorded the 1997–1998 Umbria Marche earthquake sequence. The compiled velocity measurements provide data for 51 of the 101 sites. For the remaining sites, the average seismic velocity in the upper 30 m (Vs30) is estimated using a hybrid approach. For young Quaternary alluvium, Vs30 an existing empirical relationship for California sites by Wills and Clahan (2006) is used, which we justify by validating this relationship against Italian data. For Tertiary Limestone and Italian Mesozoic rocks, empirical estimates of Vs30 are developed using the available data. This work is also presented in Scasserra et al. (2008: JEE, in review).
机译:已经编制了101个意大利地面运动站的现场条件的数据集,其中编制了包括地质特征和地震速度。地质表征主要来自eNEL的局部地质研究,包括详细的映射和横截面。对于缺乏如此详细地质特征的网站,使用了Servio Geologico D'Italia的地质图。从文献中提取地震速度以及33个网站的咨询工程师,地质学家和公共机构的文件。利用的数据来源包括后地震现场调查(Friuli和Irpinia事件),微微响应研究和研究人员或咨询工程师/地质学家进行的杂项调查。作者使用了录制了1997-1998翁瑞海地震序列的18个站点的表面波(SASW)方法的受控源光谱分析来测量额外的地震速度。编译的速度测量为101个站点的51提供数据。对于剩余的位置,使用混合方法估计上30M(VS30)中的平均地震速度。对于年轻的第四纪alluvium,VS30使用遗嘱和Clahan(2006)的加州地点的现有经验关系,我们通过验证这种与意大利数据的关系来证明。对于第三次石灰岩和意大利中生代岩石,使用可用数据开发VS30的实证估计。这项工作也在Scasserra等人中介绍。 (2008年:Jee,在审查中)。

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