Sea-level variability modulates plate thickness at mid-ocean ridges, which paces normal fault spacing and produces the observed 41 ky and 100 ky spectral peaks in abyssal hill topography.
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How sea level paces faulting at fast-spreading mid-ocean ridges
Sea-level variability modulates plate thickness at mid-ocean ridges, which paces normal fault spacing and produces the observed 41 ky and 100 ky spectral peaks in abyssal hill topography.