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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2022
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| Materias: | |
| 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 |