The Mechanics of Earthquake Fault Formation: Stress, Failure, and Fault-Zone Evolution
Introduction Earthquake faults are not random cracks in the crust; they are the expression of deep-seated mechanical processes operating under the framework of plate tectonics. The lithosphere is segmented into rigid plates that move at rates of a few centimeters per year, generating long-term stress accumulation at their boundaries and interiors. When this stress exceeds…