Slow Slip as an Indicator of Fault Stress Criticality
Abstract Fault regions inferred to be slowly slipping are interpreted to accommodate much of tectonic plate motion aseismically and potentially serve as barriers to earthquake rupture. Here, we build on prior work using simulations of earthquake sequences with enhanced dynamic fault weakening to sho...
| الحاوية / القاعدة: | Geophysical Research Letters |
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| المؤلف الرئيسي: | |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Wiley
2024-06-01
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1029/2023GL107356 |