Figure 7
From: Long-lived compositional heterogeneities in magma chambers, and implications for volcanic hazard
(a) Temporal evolution of standard deviation (σ) of composition (andesite wt%). (b) Temporal evolution of slopes of σ. (c) Semi-log plot of rate of σ. (d) Time series for maximum finite time Lyapunov exponent (FTLE). (e) Time series for silica (wt%) at Lagrangian tracer points (P1–P6 displayed in Fig. 1) for case #1. (f) Time series for silica (wt%) at Lagrangian tracer points for case #3.
