Figure 3 | Scientific Reports

Figure 3

From: The geodynamic origin of Los Humeros volcanic field in Mexico: insights from numerical simulations

Figure 3

Time series showing modeling results with dual thermal anomalies of 10, 15 and 20 km in diameter and a ΔT = 100 °C, 140 °C, and 200 °C and extensional background strain rates of 1.585–4.756–7.927 × 10–16 s−1. Time snapshots marked with a gray background depict the moment of the secondary thermal anomaly addition. The secondary thermal anomaly has the same properties as the initially set up. All models are integrated 1 Myr in time.

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