Detailed nucleation process and mechanism of the July 2019 Mw 6.4
Ridgecrest, California earthquake
Abstract
We utilized the Match&Locate method to characterize the detailed
spatial and temporal evolution of earthquakes before the July 2019 Mw
6.4 Ridgecrest, California earthquake. The Mw 6.4 mainshock was preceded
by 40 foreshocks within ~2 h (on July 4, 2017 from
15:35:29 to 17:32:52, UTC). The largest foreshock (M 4.0) separates the
foreshock activity into two stages with different nucleation mechanisms.
A swarm of repeating earthquakes occurred before the M 4.0 event,
implying the earthquake sequence initiated from an aseismic slip
process. The majority of aftershocks of the M 4.0 event as well as the
Mw 6.4 mainshock, occurred within regions of increasing Coulomb stress,
indicating that they were triggered by stress transfer. Our observations
demonstrate that neither the preslip model nor the cascade model can
explain the entire nucleation process of the Mw 6.4 mainshock. Instead,
both mechanisms govern the nucleation process, but at different stages.