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Detecting long-lasting transients of earthquake activity on a fault system by monitoring apparent stress, ground motion and clustering
Damaging earthquakes result from the evolution of stress in the brittle upper-crust, but the understanding of the mechanics of faulting cannot be achieved by only studying the large ones, which are rare. Considering a fault as a complex system, microearthquakes allow to set a benchmark in the system...
Uloženo v:
| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2019
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6838128/ https://ncbi.nlm.nih.gov/pubmed/31700092 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-52756-8 |
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