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These are transcurrent faults, usually at 90o to the main Mid-Ocean Ridge (MOR). One wall is commonly higher than the other in a systemic fashion.

It may be that the great Alpine Fault in New Zealand, about 500 km long, is a transcurrent fault of the Pacific MOR, much displaced.

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Q: The fracture zones that offset portions of mid-ocean ridges are examples of what type of boundary?
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