Exciting news! We're transitioning to the Statewide California Earthquake Center. Our new website is under construction, but we'll continue using this website for SCEC business in the meantime. We're also archiving the Southern Center site to preserve its rich history. A new and improved platform is coming soon!

Poster #167, Fault and Rupture Mechanics (FARM)

Unraveling scaling properties of slow slip events in 3D simulations of fault slip

Luca Dal Zilio, Nadia Lapusta, & Jean-Philippe Avouac
Poster Image: 

Poster Presentation

2020 SCEC Annual Meeting, Poster #167, SCEC Contribution #10607 VIEW PDF
Large megathrust faults produce a wide spectrum of slip modes, ranging from earthquakes to slow-slip events (SSEs). SSEs appear to have slip mechanisms similar to those of regular (fast) earthquakes and are often located in neighboring regions of the seismogenic zone. However, whether SSEs and regular earthquakes arise from similar failure mechanisms, and how different slip behaviors are separated in space and time, are still a matter of debate. We examine the scaling properties of SSEs using 3D dynamic simulations of frictional sliding in fault model of a velocity-weakening fault strip surrounded by velocity-strengthening areas on a rate-and-state fault with inelastic dilatancy and fluid ov...erpressure. Simulated SSEs follow the Gutenberg-Richter law and obey a cubic moment-duration scaling law — similar to that of fast (regular) earthquakes — as observed in Cascadia. In contrast to conventional and widely used assumptions of magnitude-invariant rupture velocities and stress drops, both simulated and natural SSEs have rupture velocities and stress drops that increase with event magnitudes. The success of our model in reproducing a realistic sequence of SSEs provides an excellent match to a number of observations collected along the Cascadia megathrust and indicates that rate-and-state friction combined with pore fluids effects is a plausible physical mechanism for SSEs.