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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...

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Detalles Bibliográficos
Autores principales: Dumont, Quentin, Cayol, Valérie, Froger, Jean-Luc, Peltier, Aline
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