Towards a microzonation of the Greater Beirut area: an instrumental approach combining earthquake and ambient vibration recordings |
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| Authors: | Marleine Brax Pierre-Yves Bard Anne-Marie Duval Etienne Bertrand Muhsin-Elie Rahhal Rachid Jomaa Cécile Cornou Christophe Voisin Alexandre Sursock |
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| Institution: | 1.National Council for Scientific Research, CNRS,Achrafieh, Beirut,Lebanon;2.IFSTTAR, CNRS, IRD,ISTerre, Université Grenoble Alpes,Grenoble,France;3.Cité des Mobilités,CEREMA,Bron,France;4.Laboratoire de Nice,CEREMA,Nice,France;5.Faculté d’ingénierie ESIB,Université Saint Joseph USJ,Mar Roukos, Mkalles,Lebanon |
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| Abstract: | Lebanon is situated on the 1000 km long Levant transform fault that separates the Arabic from the African tectonic plates. In Lebanon, the Levant fault splits up into a set of ramifications that had, in the past, generated major destructive earthquakes causing a lot of destruction and thousands of casualties. The most devastating one was the 551 A.D. offshore earthquake that destroyed Beirut, the capital of Lebanon. This paper presents a site effect study in Beirut, aimed at proposing a framework for future microzonation works in the city. It includes two complementary parts. A 6-month, temporary seismological experiment was first conducted to estimate the site response at 10 sites sampling the main geological units of Beirut on the basis of local and regional earthquake recordings. This spatially sparse information was then complemented by a large number (615) of microtremor measurements covering the Beirut municipality and part of its suburbs with a 400 m dense grid. The recordings were analysed with the standard site-to-reference and horizontal-to-vertical spectral ratio methods for earthquake recordings, and the horizontal-to-vertical ratio for ambient noise recordings. Significant ground motion amplification effects (up to a factor of 8) are found in a few areas corresponding to recent deposits. The consistency between results from earthquake and microtremor recordings allows proposing a map of the resonance frequencies within the city and its suburbs, with frequencies ranging from 0.5 to 5 Hz for the deepest deposits, and 5–10 Hz for shallow areas. Finally, the results are discussed and a way to combine the results obtained from the temporary stations to the great number of recordings coming from the permanent Lebanese network is proposed. |
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