S Yabe, S Ide - Journal of Geophysical Research: Solid Earth, 2017 - Wiley Online Library
Geological faults have frictional heterogeneity. Here we investigate the slip behavior of such heterogeneous faults in the simplest situation, simulating antiplane shear slip along an …
P Senatorski - Pure and applied Geophysics, 2020 - Springer
Abstract The Gutenberg–Richter (G–R) relationship can be derived as the Gibbs distribution. For a given earthquake set (all earthquakes in a given region, time period, magnitude range …
H Perfettini, A Molinari - Journal of Geophysical Research: Solid …, 2023 - Wiley Online Library
We consider a model where an unstable frictional region, governed by rate and state friction, interacts with a viscous zone with Newtonian rheology. The system is loaded at distance …
R Sakamoto, Y Tanaka - Journal of Geophysical Research …, 2022 - Wiley Online Library
Tidal triggering of tectonic tremors has been observed at plate boundaries around the circum‐Pacific region. It has been reported that the response of tremors to tidal stress during …
We explore with numerical simulations basic physical conditions leading to key observed features of non-volcanic tremor (NVT) in relation to slow slip events (SSEs) and earthquakes …
H Aochi, S Ide - Earth, Planets and Space, 2017 - Springer
Quasi-static numerical simulations of slip along a fault interface characterized by multiscale heterogeneity (fractal patch model) are carried out under the assumption that the …
P Senatorski - Physics of the Earth and Planetary Interiors, 2017 - Elsevier
The earthquake frequency-magnitude relationship is considered in the maximum entropy principle (MEP) perspective. The MEP suggests sampling with constraints as a simple …
F Smaï, H Aochi - Procedia Computer Science, 2017 - Elsevier
A problem of quasi-static growth of an arbitrary shaped-crack along an interface requires many times of iterations not only for finding a spatial distribution of discontinuity but also for …