Spatiotemporal evolution of deep fault slip and its coupled dynamic loading influence zone

Key Points

• Observed fault slip exhibits significant temporal changes influenced by dynamic loading, affecting surrounding geological systems.
• Key metrics show a clear correlation between fault slip rates and dynamic loading forces over various geological regions.
• Analysis of geological records across multiple depths reveals spatiotemporal evolution patterns in faulting behavior.
• These findings may enable improved predictions in seismic risk assessment, particularly in influence zones around faults.