Figure 1
From: Long-lived compositional heterogeneities in magma chambers, and implications for volcanic hazard

Magma chamber domain and initial setup. P1-P6 are Lagrangian tracing points (see Fig. 7e,f below).
From: Long-lived compositional heterogeneities in magma chambers, and implications for volcanic hazard

Magma chamber domain and initial setup. P1-P6 are Lagrangian tracing points (see Fig. 7e,f below).