Earth:Afterslip
From HandWiki
An afterslip is a slipping motion along a fault that occurs over months to years, after an earthquake.[1] Afterslips can either take place as a gradual movement (slow-sip) that doesn't create enough energy to set out seismic waves, or as an earthquake.[2]
References
- ↑ Qiu, Qiang; Feng, Lujia; Hermawan, Iwan; Hill, Emma M. (July 2019). "Coseismic and Postseismic Slip of the 2005 M w 8.6 Nias-Simeulue Earthquake: Spatial Overlap and Localized Viscoelastic Flow" (in en). Journal of Geophysical Research: Solid Earth 124 (7): 7445–7460. doi:10.1029/2018JB017263. ISSN 2169-9313. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2018JB017263.
- ↑ "Earthquake Processes and Effects". https://earthquake.usgs.gov/research/eqproc/posteqmotions.php#:~:text=Many%20aftershocks%20occur%20on%20the,slip%20that%20is%20not%20felt..
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