Broadscale postseismic gravity change following the 2011 Tohoku-Oki earthquake and implication for deformation by viscoelastic relaxation and afterslip

The analysis of GRACE gravity data revealed postseismic gravity increase by 6 μGal over a 500 km scale within a couple of years after the 2011 Tohoku-Oki earthquake, which is nearly 40–50% of the coseismic gravity change. It originates mostly from changes in the isotropic component corresponding to...

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Detalles Bibliográficos
Autores principales: Han, Shin-Chan, Sauber, Jeanne, Pollitz, Fred
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BlackWell Publishing Ltd 2014
Materias:
Research Letters
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4373167/
https://www.ncbi.nlm.nih.gov/pubmed/25821272
http://dx.doi.org/10.1002/2014GL060905

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4373167/
https://www.ncbi.nlm.nih.gov/pubmed/25821272
http://dx.doi.org/10.1002/2014GL060905

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