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Finite Fault Source Model for Ground Motion near Fault Zone

 Finite Fault Source Model for Ground Motion near Fault Zone
Autor(en): , ORCID, , , ORCID
Beitrag für IABSE Congress: Bridges and Structures: Connection, Integration and Harmonisation, Nanjing, People's Republic of China, 21-23 September 2022, veröffentlicht in , S. 854-862
DOI: 10.2749/nanjing.2022.0854
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Ground motion is categorized into near fault zone and across fault zone where impulsive component is included. The impulsive component usually causes larger damage than that by far-fault ground mot...
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Bibliografische Angaben

Autor(en): (Tongji University, Shanghai, China)
ORCID (Tongji University, Shanghai, China)
(Tongji University, Shanghai, China)
(Sichuan Highway Planning, Survey, Design and Research Institute Ltd., Chengdu, China)
ORCID (Universitat Politècnica de Catalunya BarcelonaTech, Barcelona, Spain)
(Universidad de Castilla-La Mancha, Ciudad Real, Spain)
Medium: Tagungsbeitrag
Sprache(n): Englisch
Tagung: IABSE Congress: Bridges and Structures: Connection, Integration and Harmonisation, Nanjing, People's Republic of China, 21-23 September 2022
Veröffentlicht in:
Seite(n): 854-862 Anzahl der Seiten (im PDF): 9
Seite(n): 854-862
Anzahl der Seiten (im PDF): 9
DOI: 10.2749/nanjing.2022.0854
Abstrakt:

Ground motion is categorized into near fault zone and across fault zone where impulsive component is included. The impulsive component usually causes larger damage than that by far-fault ground motion. To build a Benchmark model platform for cable-stayed bridges across-fault region for comparative analysis, the paper proposes a way combining the finite fault source model. In the paper, the finite fault source model was conducted based on the site Qiongshan earthquake. After the geological structural parameters were determined, forward modeling of near site earthquake was carried out, and the observation points were obtained using numerical simulation. Then, the analysis results were compared with the pulse characteristic parameters of similar grade of recording ground motion. Additionally, the ground motion near-fault region was analyzed to validate the finite fault source model.

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