Seismic imaging of a lithospheric-scale magma plumbing system.
3 low velocity bodies in the mid-crust beneath the active volcanic arc and backarc.
The mid-crustal magma reservoir beneath the Cerro Galan Caldera contains ∼22% melt.
Slow upper mantle velocities are indicative of a MASH zone with class="mathmlsrc">class="formulatext stixSupport mathImg" data-mathURL="/science?_ob=MathURL&_method=retrieve&_eid=1-s2.0-S0012821X1630557X&_mathId=si1.gif&_user=111111111&_pii=S0012821X1630557X&_rdoc=1&_issn=0012821X&md5=0082e48d206fd666917f89ea3f995f59" title="Click to view the MathML source">∼4–9%class="mathContainer hidden">class="mathCode"> melt.
A large MASH zone underlies the southern Puna Plateau as a result of delamination.