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.
Glacial cycles drive variations in the production of oceanic crust
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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.