Simulation Results for "Subducted Seamounts Promote Slow and Fast Slip throughout the Seismic Cycle"

Subset of data shown in various figures throughout the paper. simulations_fig2 is a structured array consisting of 3 simulations (A,B,C) shown in Fig. 2 and 3: simulation name x: horizontal distance [km] y: vertical distance [km]t: time [s] v: slip speed [m/s] slip: cummulative slip [m] tau: shear stress [Pa] es: normal stress [Pa] catalog_Fig3 is a structured array consisting of an earthquake catalog of the simulations as shown in Fig. 3: x: horizontal distance [km] t: time [s] Dx: horizontal location seamount center [km] sig0: background normal stress [MPa] stresscontrast: normal stress contrast [-] seamount_nucleation: earthquakes nucleate at seamount [0 or 1] PR: partial ruptures at the seamount [0 or 1] ST: slow transients preceding seamount earthquakes [0 or 1] nucleation_idx: nucleation patches for each earthquake [-] rupture_idx: rupture extent for each earthquake [-] Tn_simulation: recurrence time for each earthquake [yrs] Tn_theory: time-to-nucleation on the fault, see Eq. 8 [yrs] v_max: log10 of maximum slip speed on the fault [m/s] v_sigweak: log10 of slip speed at sigma_weak [m/s] simulation_fig8 is a subset of the simulation as shown in Fig. 8d: x: horizontal distance [km] y: vertical distance [km]t: time [s] v: slip speed [m/s] slip: cummulative slip [m] tau: shear stress [Pa] es: normal stress [Pa]