Revealing the spatiotemporal complexity of the magnitude distribution and b-value during an earthquake sequence

The Magnitude–Frequency-Distribution (MFD) of earthquakes is typically modeled with the (tapered) Gutenberg–Richter relation. The main parameter of this relation, the b-value, controls the relative rate of small and large earthquakes. Resolving spatiotemporal variations of the b-value is critical to...

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Detalles Bibliográficos
Autores principales: Herrmann, Marcus, Piegari, Ester, Marzocchi, Warner
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9424211/
https://www.ncbi.nlm.nih.gov/pubmed/36038553
http://dx.doi.org/10.1038/s41467-022-32755-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9424211/
https://www.ncbi.nlm.nih.gov/pubmed/36038553
http://dx.doi.org/10.1038/s41467-022-32755-6

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