Dynamics of earthquake nucleation process represented by the Burridge-Knopoff model

TL;DR

This study analyzes earthquake nucleation using the one-dimensional Burridge-Knopoff model with rate- and state-dependent friction, identifying key nucleation lengths and stages, and discussing implications for real seismicity.

Contribution

It provides a detailed characterization of the nucleation process, including the identification of nucleation lengths and stages, within the BK model under RSF law, and discusses continuum limits.

Findings

Nucleation lengths L_sc and L_c depend on model parameters.

Nucleation stages include quasi-static, acceleration, and rupture phases.

Initial sliding velocity is extremely slow, reaching detectable levels during acceleration.

Abstract

Dynamics of earthquake nucleation process is studied on the basis of the one-dimensional Burridge-Knopoff (BK) model obeying the rate- and state-dependent friction (RSF) law. We investigate the properties of the model at each stage of the nucleation process, including the quasi-static initial phase, the unstable acceleration phase and the high-speed rupture phase or a mainshock. Two kinds of nucleation lengths L_sc and L_c are identified and investigated. The nucleation length L_sc and the initial phase exist only for a weak frictional instability regime, while the nucleation length L_c and the acceleration phase exist for both weak and strong instability regimes. Both L_sc and L_c are found to be determined by the model parameters, the frictional weakening parameter and the elastic stiffness parameter, hardly dependent on the size of an ensuing mainshock. The sliding velocity is extremely slow in the initial phase up to L_sc, of order the pulling speed of the plate, while it reaches a detectable level at a certain stage of the acceleration phase. The continuum limits of the results are discussed. The continuum limit of the BK model lies in the weak frictional instability regime so that a mature homogeneous fault under the RSF law always accompanies the quasi-static nucleation process. Duration times of each stage of the nucleation process are examined. The relation to the elastic continuum model and implications to real seismicity are discussed.