Supplementary material for “Regional controls on magma ascent and storage in
volcanic arcs”
Figure S1: Depths of magma storage in function of the convergence velocity (same
legend as Figure 4). (a) At the 70 volcanoes individually, the volcanic regions being
color-coded similarly to Figure 2. (b) Cumulative histograms of the proportion of shallow
and deep reservoirs in function of ranges of convergence velocities. In this and in the
following figures a horizontal orange boxes indicates a lack of a correlation whereas a
non-horizontal box suggests the presence of a correlation.
Figure S2: Same as Figure S1 but in function of the subduction velocity.
1
Figure S3: Same as Figure S1 but in function of the vertical descent velocity.
Figure S4: Same as Figure S1 but in function of the slab age.
Figure S5: Same as Figure S1 but in function of the slab dip angle.
2
Figure S6: Same as Figure S1 but in function of the current duration of the subduction.
Figure S7: Same as Figure S1 but in function of the parameter ϕ representative of the slab
temperature.
Figure S8: Same as Figure S1 but in function of the upper-plate surface heat flux.
3
4
5
Table 1: Data used in this study (followed by the corresponding references).
6
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