Rain and small earthquakes maintain a slow-moving landslide in a persistent critical state

In tectonically active mountain belts, landslides contribute significantly to erosion. Statistical analysis of regional inventories of earthquake-triggered-landslides after large earthquakes (Mw > 5.5) reveal a complex interaction between seismic shaking, landslide material, and rainfall. However...

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Detalles Bibliográficos
Autores principales: Bontemps, Noélie, Lacroix, Pascal, Larose, Eric, Jara, Jorge, Taipe, Edu
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005893/
https://www.ncbi.nlm.nih.gov/pubmed/32034136
http://dx.doi.org/10.1038/s41467-020-14445-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005893/
https://www.ncbi.nlm.nih.gov/pubmed/32034136
http://dx.doi.org/10.1038/s41467-020-14445-3

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