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1. On factors controlling precursor slip fronts in the laboratory and their relation to slow slip events in nature: LABORATORY SLOW SLIP EVENTS

   https://doi.org/10.1002/2017GL072538  

   Selvadurai, Paul A. ; Glaser, Steven D. ; Parker, Jessica M. ( March 2017 , Geophysical Research Letters)
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

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   Lipovsky, Bradley Paul ; Dunham, Eric M. ( April 2017 , Journal of Geophysical Research: Earth Surface)
3. Expedition 405 Scientific Prospectus: Tracking Tsunamigenic Slip Across the Japan Trench (JTRACK)

   Kodaira, S. ; Conin, M. ; Fulton, P. ; Kirkpatrick, J. ; Regalla, C. ; Ujiie, K. ; Okutsu, N. ; Maeda, L. ; Toczko, S. ; Eguchi, N. ( July 2023 , Scientific prospectus)

   The 11 March 2011 M 9.0 Tohoku-oki earthquake was one of the largest earthquakes ever recorded and was accompanied by a devastating tsunami. Slip during the earthquake was exceptionally large at shallow depth on the plate boundary fault, which was one of the primary factors that contributed to the extreme tsunami amplitudes that inundated the coast of Japan. International Ocean Discovery Program Expedition 405 aims to investigate the conditions and processes that facilitated the extremely shallow slip on the subduction interface in the 2011 Tohoku-oki earthquake. Proposed work includes coring and logging operations at two sites in a transect across the trench. The first site, located within the overriding plate, will access the fault zone in the region of large shallow slip, targeting the plate boundary décollement, overlying frontal prism, and subducted units cut by the décollement. The second site, located on the Pacific plate, will access the undisturbed sedimentary and volcanic inputs to the subduction zone. A borehole observatory will be installed into the décollement and surrounding rocks to provide measurements of the temperature in and around the fault over the following several years. Sampling, geophysical logs, and the observatory temperature time series will document the compositional, structural, mechanical, and frictional properties of the rocks in the décollement and adjacent country rock, as well as the hydrogeologic structure and pore fluid pressure of the fault zone and frontal prism—key properties that influence the effective stress to facilitate earthquake slip and potential for large slip. Results from Expedition 405 will address fundamental questions about earthquake slip on subduction zones that may directly inform earthquake and tsunami hazard assessments around the world. 

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4. 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)
5. 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)

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