Fault zones cause a rotation of the background stress field and can induce plastic deformations
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منابع مشابه
Earthquake ruptures modulated by waves in damaged fault zones
Faults are usually surrounded by damaged zones of lower elastic moduli and seismic wave velocities than their host rocks. If the interface between the damaged rocks and host rocks is sharp enough, earthquakes happening inside the fault zone generate reflected waves and head waves, which can interact with earthquake ruptures and modulate rupture properties such as rupture speed, slip rate, and r...
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