GPS source solution of the 2004 Parkfield earthquake

We compute a series of finite-source parameter inversions of the fault rupture of the 2004 Parkfield earthquake based on 1 Hz GPS records only. We confirm that some of the co-seismic slip at shallow depth (<5 km) constrained by InSAR data processing results from early post-seismic deformation. We...

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Detalles Bibliográficos
Autores principales: Houlié, N., Dreger, D., Kim, A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3894560/
https://www.ncbi.nlm.nih.gov/pubmed/24434939
http://dx.doi.org/10.1038/srep03646

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3894560/
https://www.ncbi.nlm.nih.gov/pubmed/24434939
http://dx.doi.org/10.1038/srep03646

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