Final answer:
Strike-slip faults are most commonly associated with transform plate margins, where tectonic plates slide past one another horizontally.
Step-by-step explanation:
Strike-slip faults are commonly found along transform plate margins where the motion between tectonic plates is primarily horizontal, meaning the plates slide past one another. In contrast, convergent boundaries involve plates moving toward each other, often resulting in one plate being forced under another, and divergent boundaries are characterized by plates moving away from each other, such as at mid-ocean ridges. Since strike-slip faults involve lateral movement, they are a hallmark of transform boundaries and can result in shallow earthquakes but typically do not have associated volcanic activity.