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]