Del Gaudio, Sergio (2014) strong motion simulations with empirical Green's functions: methodology and application to the 2009 L'Aquila earthquake. [Tesi di dottorato]
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| Item Type: | Tesi di dottorato |
|---|---|
| Resource language: | English |
| Title: | strong motion simulations with empirical Green's functions: methodology and application to the 2009 L'Aquila earthquake |
| Creators: | Creators Email Del Gaudio, Sergio sergio.delgaudio@unina.it |
| Date: | 31 March 2014 |
| Number of Pages: | 112 |
| Institution: | Università degli Studi di Napoli Federico II |
| Department: | Fisica |
| Scuola di dottorato: | Scienze fisiche |
| Dottorato: | Rischio sismico |
| Ciclo di dottorato: | 26 |
| Coordinatore del Corso di dottorato: | nome email Zollo, Aldo aldo.zollo@unina.it |
| Tutor: | nome email Festa, Gaetano UNSPECIFIED |
| Date: | 31 March 2014 |
| Number of Pages: | 112 |
| Keywords: | seismology;ground motion simulations;L'Aquila earthquake |
| Settori scientifico-disciplinari del MIUR: | Area 02 - Scienze fisiche > FIS/06 - Fisica per il sistema terra e il mezzo circumterrestre |
| Aree tematiche (7° programma Quadro): | AMBIENTE (INCLUSO CAMBIAMENTO CLIMATICO) > Proteggere i cittadini dai rischi ambientali |
| Date Deposited: | 15 Apr 2014 16:35 |
| Last Modified: | 23 Jan 2015 11:54 |
| URI: | http://www.fedoa.unina.it/id/eprint/10026 |
Collection description
In the last ten years, thanks to the great advances in computer science and to the huge improvements of strong motion networks, our knowledge of the Earth interior and its related phenomena greatly increased. This improvement directly comes from the amount of collected data, such as recorded signals during earthquakes, that are now shared by worldwide databanks. We observe an earthquake rupture from the elastic waves produced by a sudden release of energy in the Earth's crust: the seismic waves. These waves bring informations on both their source and all the features of the medium that they have passed through. The aim of this thesis was to build up and test a robust methodology to produce synthetic records which are as similar as possible to the real ones. My final goal is to perform ground motion predictions with this technique to obtain scenario simulations for probable future earthquakes in active seismic regions.
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