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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6823

Authors: Calderoni, G.*
Rovelli, A.*
Di Giovambattista, R.*
Title: Large amplitude variations recorded by an on-fault seismological station during the L’Aquila earthquakes: evidence for a complex fault-induced site effect
Issue Date: 17-Dec-2010
Keywords: L'Aquila earthquakes
seismic trapped waves
fault zone properties
Abstract: This study is focused on amplification effects observed at an on-fault station, FAGN, near L’Aquila. The difference in amplitude, compared to nearby stations, is extremely large for some particular events and neigligible for others of the same seismic sequence. FAGN is located on the S. Demetrio fault (Vezzani and Ghisetti, 1998) and the presence of the fault zone beneath the station could play a role on the observed amplifications (Davis et al., 2000; Cultrera et al., 2003; Karabulut and Bouchon, 2007). The fault-guided propagation effect is investigated through numerical modeling and analytical solutions by Ben-Zion and Aki (1990) and Ben-Zion (1998).
Appears in Collections:04.06.09. Waves and wave analysis
01.02.05. Wave propagation
Conference materials
04.01.99. General or miscellaneous
04.02.06. Seismic methods
04.06.99. General or miscellaneous
04.06.01. Earthquake faults: properties and evolution
04.06.04. Ground motion

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Poster_AGU_2010.pdfPoster24.43 MBAdobe PDFView/Open


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