Abstract. We examine the dynamical behaviour of the phenomenological Burridge-Knopoff-like model with one and two blocks, where the friction term is supplemented by the time delay τ and the variable friction strength c. Time delay is assumed to reflect the initial quiescent period of the fault healing, considered to be a function of history of sliding. Friction strength parameter is proposed to mimic the impact of fault gouge thickness on the rock friction. For the single-block model, interplay of the introduced parameters c and τ is found to give rise to oscillation death, which corresponds to aseismic creeping along the fault. In the case of two blocks, the action of c 1 , c 2 , τ 1 and τ 2 may result in several effects. If both blocks exhibit oscillatory motion without the included time delay and frictional strength parameter, the model undergoes transition to quasiperiodic motion if only c 1 and c 2 are introduced. The same type of behaviour is observed when τ 1 and τ 2 are varied under the condition c 1 = c 2 . However, if c 1 , and τ 1 are fixed such that the given block would lie at the equilibrium while c 2 and τ 2 are varied, the (c 2 , τ 2 ) domains supporting quasiperiodic motion are interspersed with multiple domains admitting the stationary solution. On the other hand, if (c 1 , τ 1 ) warrant oscillatory behaviour of one block, under variation of c 2 and τ 2 the system's dynamics is predominantly quasiperiodic, with only small pockets of (c 2 , τ 2 ) parameter space admitting the periodic motion or equilibrium state. For this setup, one may also find a transient chaos-like behaviour, a point corroborated by the positive value of the maximal Lyapunov exponent for the corresponding time series.