| Registro completo |
| Provedor de dados: |
ArchiMer
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| País: |
France
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| Título: |
Comment on "Zemmouri earthquake rupture zone (M-w 6.8, Algeria): Aftershocks sequence relocation and 3D velocity model" by A. Ayadi et al.
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| Autores: |
Deverchere, Jacques
De Lepinay, Bernard Mercier
Cattaneo, Antonio
Strzerzynski, Pierre
Calais, Eric
Domzig, Anne
Bracene, Rabah
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| Data: |
2010-04
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| Ano: |
2010
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| Palavras-chave: |
Boumerdès-Zemmouri earthquake
Deformation
Kinematics
Margin
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| Resumo: |
Although often difficult to characterize, the relationship between a seismic rupture, its aftershock sequence, and cumulative subsurface or surface faulting or folding is an important challenge to modern seismology and seismotectonics. Among other benefits, it helps document fault length, slip, and magnitude relationships, reconstruct the evolution of the rupture process through historical and prehistorical times and identify the complexity of the deformation in its path toward the surface. This approach is a prerequisite to any seismic hazard assessment but is particularly difficult for faults whose surface trace projects offshore. A specific effort to identify and quantify the source parameters of large earthquakes in coastal areas is therefore needed, not only in subduction zones but also in areas of slow rate and/or diffuse deformation.
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| Tipo: |
Text
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| Idioma: |
Inglês
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| Identificador: |
http://archimer.ifremer.fr/doc/00003/11440/7994.pdf
DOI:10.1029/2008JB006190
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| Editor: |
Amer Geophysical Union
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| Relação: |
http://archimer.ifremer.fr/doc/00003/11440/
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| Formato: |
application/pdf
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| Fonte: |
Journal Of Geophysical Research-solid Earth (0148-0227) (Amer Geophysical Union), 2010-04 , Vol. 115 , N. B04320 , P. 1-6
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| Direitos: |
2010. American Geophysical Union. All Rights Reserved.
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