Linking megathrust earthquakes to brittle deformation in a fossil accretionary complex

Seismological data from recent subduction earthquakes suggest that megathrust earthquakes induce transient stress changes in the upper plate that shift accretionary wedges into an unstable state. These stress changes have, however, never been linked to geological structures preserved in fossil accre...

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Detalles Bibliográficos
Autores principales: Dielforder, Armin, Vollstaedt, Hauke, Vennemann, Torsten, Berger, Alfons, Herwegh, Marco
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4491836/
https://www.ncbi.nlm.nih.gov/pubmed/26105966
http://dx.doi.org/10.1038/ncomms8504

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4491836/
https://www.ncbi.nlm.nih.gov/pubmed/26105966
http://dx.doi.org/10.1038/ncomms8504

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