Constant strain accumulation rate between major earthquakes on the North Anatolian Fault

Earthquakes are caused by the release of tectonic strain accumulated between events. Recent advances in satellite geodesy mean we can now measure this interseismic strain accumulation with a high degree of accuracy. But it remains unclear how to interpret short-term geodetic observations, measured o...

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Detalles Bibliográficos
Autores principales: Hussain, Ekbal, Wright, Tim J., Walters, Richard J., Bekaert, David P. S., Lloyd, Ryan, Hooper, Andrew
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5895838/
https://www.ncbi.nlm.nih.gov/pubmed/29643366
http://dx.doi.org/10.1038/s41467-018-03739-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5895838/
https://www.ncbi.nlm.nih.gov/pubmed/29643366
http://dx.doi.org/10.1038/s41467-018-03739-2

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