Seafloor displacements across the mid-ocean ridge eruption cycle modulated by mush zone viscosity - supplementary materials

Supplements for Boulze & Olive, submitted We provide tables that document horizontal and vertical seafloor normalized velocities for slow, intermediate, and slow ridges, as a function of mush viscosity. Mush viscosities range from 10^16 to 10^18 Pa.s, and normalized velocities are reported for cross-axis distances spanning from −10 km to +10 km relative to the ridge axis. These tables allow detailed examination of the sensitivity of seafloor deformation to rheological variations in the mush zone.