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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SPH simulations produce a scaling relation showing giant impacts heat the core by ~3000 K on average with strong thermal stratification, allowing the core to reach an adiabatic state 290 Myr later consistent with geodynamo evidence.
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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.
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A scaling relation for core heating by giant impacts and implications for dynamo onset
SPH simulations produce a scaling relation showing giant impacts heat the core by ~3000 K on average with strong thermal stratification, allowing the core to reach an adiabatic state 290 Myr later consistent with geodynamo evidence.