Figure 4
From: The geodynamic origin of Los Humeros volcanic field in Mexico: insights from numerical simulations
Time series showing modeling results with a series of three thermal anomalies of 15 km in diameter, a ΔT = 120 °C, 140 °C, and 160 °C and constant extensional background strain rates of 7.927 × 10–16 s−1. Time snapshots marked with a gray background depict the moment of the secondary and tertiary thermal anomaly additions. All thermal anomalies have the same properties as initially setup; all models are integrated 1 Myr in time.
