Figure 3
From: Triggering of eruptions at Axial Seamount, Juan de Fuca Ridge
2D slices through the 3D model space show the implemented Young’s modulus, viscosity structure, thermal gradient, and thermal conductivity for each tested rheology: Non-TD Elastic (no temperature dependence); Non-TD Viscoelastic; Full TD, a viscoelastic implementation that includes a temperature-dependent Young’s Modulus and temperature-dependent viscosity; and Full TD + Hydrothermal, which incorporates increased thermal conductivity in the brittle portions of the model space. Magma reservoir is shown as the white half ellipsoid. To view the complete model-space, refer to Supplemental Fig. S1.
