Bifurcations at the stability transition of earthquake faulting
Tectonic faults typically break in a single rupture mode within the range of styles from slow slip to dynamic earthquake failure. However, in increasingly well‐documented instances, the same fault segment fails in both slow and fast modes within a short period, as in the sequences that culminated in...
| Hoofdauteurs: | , , , , , |
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| Andere auteurs: | |
| Formaat: | Journal Article |
| Taal: | English |
| Gepubliceerd in: |
2021
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| Onderwerpen: | |
| Online toegang: | https://hdl.handle.net/10356/146197 |