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1. On the evolution of elastic properties during laboratory stick-slip experiments spanning the transition from slow slip to dynamic rupture: PRECURSORS TO THE SPECTRUM OF SLIP MODES

   https://doi.org/10.1002/2016JB013545  

   Tinti, E. ; Scuderi, M. M. ; Scognamiglio, L. ; Di Stefano, G. ; Marone, C. ; Collettini, C. ( December 2016 , Journal of Geophysical Research: Solid Earth)
2. Slow-slip events on the Whillans Ice Plain, Antarctica, described using rate-and-state friction as an ice stream sliding law: SLOW SLIP ON THE WHILLANS ICE PLAIN

   https://doi.org/10.1002/2016JF004183  

   Lipovsky, Bradley Paul ; Dunham, Eric M. ( April 2017 , Journal of Geophysical Research: Earth Surface)
3. Slip-rate-dependent friction as a universal mechanism for slow slip events

   https://doi.org/10.1038/s41561-020-0627-9  

   Im, Kyungjae ; Saffer, Demian ; Marone, Chris ; Avouac, Jean-Philippe ( October 2020 , Nature Geoscience)

   null (Ed.)
4. Interseismic Coupling and Slow Slip Events on the Cascadia Megathrust

   https://doi.org/10.1007/s00024-018-1991-x  

   Michel, Sylvain ; Gualandi, Adriano ; Avouac, Jean-Philippe ( September 2018 , Pure and Applied Geophysics)

   Abstract—In this study, we model geodetic strain accumulation along the Cascadia subduction zone between 2007.0 and 2017.632 using position time series from 352 continuous GPS stations. First, we use the secular linear motion to determine interseismic locking along the megathrust. We determine two end member models, assuming that the megathrust is either a priori locked or creeping, which differ essentially along the trench where the inversion is poorly constrained by the data. In either case, significant locking of the megathrust updip of the coastline is needed. The downdip limit of the locked portion lies * 20–80 km updip from the coast assuming a locked a priori, but very close to the coast for a creeping a priori. Second, we use a variational Bayesian Independent Component Analysis (vbICA) decomposition to model geodetic strain time variations, an approach which is effective to separate the geodetic strain signal due to non-tectonic and tectonic sources. The Slow Slip Events (SSEs) kinematics is retrieved by linearly inverting for slip on the megathrust the Independent Components related to these transient phenomena. The procedure allows the detection and modelling of 64 SSEs which spatially and temporally match with the tremors activity. SEEs and tremors occur well inland from the coastline and follow closely the estimated location of the mantle wedge corner. The transition zone, between the locked portion of the megathrust and the zone of tremors, is creeping rather steadily at the long-term slip rate and probably buffers the effect of SSEs on the megathrust seismogenic portion. 

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5. Segmentation of Shallow Slow Slip Events at the Hikurangi Subduction Zone Explained by Along‐Strike Changes in Fault Geometry and Plate Convergence Rates

   https://doi.org/10.1029/2021JB022913  

   Perez‐Silva, Andrea ; Kaneko, Yoshihiro ; Savage, Martha ; Wallace, Laura ; Li, Duo ; Williams, Charles ( January 2022 , Journal of Geophysical Research: Solid Earth)