The Owen Fracture Zone is a significant geological feature located in the Indian Ocean, specifically demarcating the boundary between the Arabian Plate and the Indian Plate. It is characterized by a series of transform faults and related features. The zone is essentially a transform boundary where tectonic plates slide past one another horizontally, which often leads to seismic activity. The Owen Fracture Zone runs generally north-south and is known for its complex structure, including various fault lines and ridges.
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