Cargando…
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...
| Autores principales: | , , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
|
| Materias: | |
| 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 |