Which outcome occurs when strike-slip faults experience sustained tectonic stress accumulation?

💡 Explanation

When strike-slip faults accumulate tectonic stress, aseismic creep and episodic tremor and slip (ETS) events occur because fault segments periodically release accumulated strain through slow slip, deep tremors, and elastic rebound. Therefore ETS events result, rather than crust formation, salinity changes, or desertification, which involve different active environmental processes.

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