The Chile Fracture Zone is a significant geological feature located off the coast of Chile in the southeastern Pacific Ocean. It is part of the larger complex of tectonic structures associated with the boundary between the Nazca Plate and the South American Plate. The fracture zone is characterized by a series of transform faults and is associated with the subduction of the Nazca Plate beneath the South American Plate, which has significant geological and seismic implications for the region.
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