Which seismic outcome characterizes regions near strike-slip faults experiencing tectonic creep?

💡 Explanation

When tectonic creep happens along strike-slip faults, continuous and slow movement releases built-up stress and energy through frequent small tremors. Therefore frequent, low-magnitude seismic tremors result, rather than high-magnitude ruptures or swarms which occur with stick-slip behavior or aseismic deformation which isn't seismic.

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