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Kane Fracture Zone : ウィキペディア英語版
Kane Fracture Zone
The Kane Fracture Zone is a medium-offset transform fault zone located on the Mid-Atlantic Ridge.〔Tucholke, Brian E.; Schouten, Hans (1988-03-01). "Kane Fracture Zone". Marine Geophysical Research 10: 1–39. doi:10.1007/BF02424659〕 It lies just to the north of the Kane Megamullion, an oceanic core complex that forms the footwall of a long-lived low-angle detachment fault.〔Dick, H. J., Tivey, M. A., & Tucholke, B. E. (2008). Plutonic foundation of a slow‐spreading ridge segment: Oceanic core complex at Kane Megamullion, 23 30′ N, 45 20′ W. Geochemistry, Geophysics, Geosystems, 9(5).〕 The Mid-Atlantic Ridge near the Kane Fracture zone (known as the MARK area) has been the focus of detailed scientific investigations, notably Expeditions 106 and 109 of the Ocean Drilling Program, as well as numerous other geological and geophysical studies.
==References==


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