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. 2015 Aug 17;5:13100. doi: 10.1038/srep13100

Figure 3. Model of the dynamics of the sill intrusion.

Figure 3

(A) “a posteriori” p.d.f. as a function of magma viscosity (η) and of the amount of liquid magma already present in the sill before the 2012–2013 episode (Vini). The red contour encloses the area with 95% of probability. The corresponding confidence bounds are delimited by the red lines. (B) Inferred magma flow rate. (C) Cumulative volume (Cum. volume) of injected magma.