Cargando…
22 years of satellite imagery reveal a major destabilization structure at Piton de la Fournaise
Volcanic activity can induce flank failure, sometimes generating large earthquakes and tsunamis. However, the failure structures have never been fully characterized and the failure mechanism is still debated. Magmatic activity is a possible trigger, either through fault slip, which might be induced...
| Autores principales: | , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2022
|
| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9098438/ https://www.ncbi.nlm.nih.gov/pubmed/35551438 http://dx.doi.org/10.1038/s41467-022-30109-w |