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 calibrated multiphase flow-geomechanics model of the Wilmington Oil Field from 1936-2020 indicates that initializing the sedimentary section with low deviatoric stress provides the best fit to historical ground deformation data and implies a shift from the previously assumed reverse-faulting regim
citing papers explorer
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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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Stress state, subsidence, and faulting in the Wilmington Oil Field, California: a multiphase flow-geomechanics modeling assessment (1936-2020)
A calibrated multiphase flow-geomechanics model of the Wilmington Oil Field from 1936-2020 indicates that initializing the sedimentary section with low deviatoric stress provides the best fit to historical ground deformation data and implies a shift from the previously assumed reverse-faulting regim