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New View of the Mid-Ocean Ridge from the Behaviour of Ridge-Axis Discontinuities

机译:从脊轴不连续行为看中海脊的新观点

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High-resolution images covering large areas of the seafloor reveal numerous discontinuities along the mid-ocean ridge. The discontinuities occur at a range of scales (10-1,000 km) and define a fundamental segmentation of seafloor spreading centres. Some are transient; others persist for millions of years, migrating along the mid-ocean ridge and disrupting the structural and geochemical character of approximately 20% of the oceanic lithosphere. Reprints. (edc)

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