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Titlebook: Earthquake Microzoning; Antoni Roca (Head of the Geological Survey),Carlos Book 2002 Springer Basel AG 2002 Earthquake mechanism.earthquak

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發(fā)表于 2025-3-21 17:18:47 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Earthquake Microzoning
編輯Antoni Roca (Head of the Geological Survey),Carlos
視頻videohttp://file.papertrans.cn/301/300902/300902.mp4
叢書名稱Pageoph Topical Volumes
圖書封面Titlebook: Earthquake Microzoning;  Antoni Roca (Head of the Geological Survey),Carlos Book 2002 Springer Basel AG 2002 Earthquake mechanism.earthquak
描述In many past and recent earthquakes it has been shown that the local conditions and, in particular, the local geology have a great influence on the observed seismic ground motion and, consequently, on the damage distribution in housing, industrial stock, and life-lines. Seismic microzoning is the usual procedure to have these local effects taken into account for engineering design and land-use planning, being a useful tool for earthquake risk mitigation. This volume presents a collection of papers mainly originated from a workshop on Seismic Microzoning, organized during the 23rd General Assembly of the European Geophysical Society (EGS) in Nice, France in April 1998. The workshop dealt with various geophysical tools for analysing the effects of the local soils of subsurface geology on seismic ground motion, namely the methods using experimental data such as microtremors, and the theoretical/numerical 1-D and 2-D modelling methods. Additional contributions discussing techniques for characterising soil properties, microzoning applications to several urban areas, and others were added to the volume to broaden this important topic.
出版日期Book 2002
關(guān)鍵詞Earthquake mechanism; earthquake; geology; geophysics; modelling; sediment; seismic; tectonics
版次1
doihttps://doi.org/10.1007/978-3-0348-8177-7
isbn_softcover978-3-7643-6652-0
isbn_ebook978-3-0348-8177-7Series ISSN 2504-3625 Series E-ISSN 2504-3633
issn_series 2504-3625
copyrightSpringer Basel AG 2002
The information of publication is updating

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Site Effects and Design Provisions: The Case of Euroseistest,tional amplification in response spectra that cannot be accounted for without reference to the lateral heterogeneity of the valley structure. Our numerical results are extensively compared with observations, which show that the additional amplification computed from the 2-D model is real and affects
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地板
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,Surface Soil Effects Study Using Short-period Microtremor Observations in Almería City, Southern Sp useful for understanding the uppermost soil characteristics and are used for soil classification. Finally, short-period microtremor observations were densely carried out in the research area and N. method (1989) was applied for determining predominant periods. Microtremors were observed at about 17
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Caracas, Venezuela, Site Effect Determination with Microtremors,h frequencies previously predicted from computation and with 1967 earthquake observations. Moreover, interpolation surfaces show that amplification (Ao) of H/V on microtremor is quite low above rock but is high on the south part of the basin. The maximum occurs over the non-urbanized zone. However t
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Seismic Zonation of Barcelona Based on Numerical Simulation of Site Effects,function and by PGA amplifications, are proposed. The numerical results are compared with those previously obtained through microtremor measurements, showing that predominant periods derived from Nakamura’s technique should be taken carefully.
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