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Long-period ground-motions for large European earthquakes, 1905-1992, and comparisons with stochastic predictions

机译:1905-1992年欧洲大地震的长期地面运动,以及与随机预测的比较

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Data from European earthquakes in the magnitude range 5 to 8 between 1905 and 1992 have been collected and collated, for distances between 200 and 3400 km. The data include both analog and digital records, with priority on wave paths traversing northern Europe. Historical analog records from Uppsala and De Bilt have been digitised, and appropriate response functions established. New estimates of seismic moments and moment magnitudes have been obtained, which together with moment magnitudes from other sources have been compared to surface wave magnitudes. The location of the largest north European earthquakes substantiate earlier suggestions that rifted regions (passive margins, rifts and grabens) may have the largest seismic potentials. A random-vibration (stochastic) model for prediction of observed peak amplitude, period and Fourier acceleration spectra has been developed and calibrated against intermediate and long-period observations. Reasonably good correspondence between predictions and observations are obtained when using a simple Brune source spectrum, new values for seismic moments and moment-magnitude relations, together with reasonable assumptions for stress drop, geometrical spreading and anelastic attenuation. The model is useful first of all for predicting broad regional averages, but as such it is robust, and it also has the potential to be used in an engineering context for predicting spectral response and peak ground accelerations. Some of the empirical data have also been studied in terms of pseudo-relative spectral velocity and compared to strong-motion response spectral prediction models established for northwestern Europe, again for low frequencies. Irrespective of these prediction models we emphasize, however, that the establishment of the data base itself has been an independent and important purpose of this study.
机译:收集并整理了1905年至1992年欧洲范围5至8级地震的数据,其距离为200至3400 km。数据包括模拟和数字记录,优先穿越北欧的波道。来自乌普萨拉和De Bilt的历史模拟记录已被数字化,并建立了适当的响应功能。获得了地震矩和矩量的新估计,并将其与其他来源的矩量一起与地表波量进行了比较。北欧最大地震的地点证实了较早的建议,即裂谷地区(被动边缘,裂谷和grab陷)可能具有最大的地震潜力。已经开发了一种随机振动(随机)模型,用于预测观测到的峰值幅度,周期和傅立叶加速度谱,并针对中长期观测进行了校准。当使用简单的Brune源谱,地震矩和矩量级关系的新值以及合理的应力降,几何扩展和非弹性衰减假设时,可以在预测和观测之间获得合理的良好对应关系。该模型首先可用于预测广泛的区域平均值,但它具有鲁棒性,并且还具有在工程环境中用于预测光谱响应和峰值地面加速度的潜力。还根据伪相对谱速度研究了一些经验数据,并将其与为西北欧洲(同样针对低频)建立的强运动响应谱预测模型进行了比较。但是,无论这些预测模型如何,我们都强调,数据库本身的建立一直是这项研究的独立且重要的目的。

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