On the decompression melting structure at volcanic arcs and back‐arc spreading centers

By J. Conder, D. Wiens, J. Morris. 2002

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Subduction-triggered magmatic pulses: A new class of plumes? (2010, background): “The 2D numerical models indicate that slab-induced mantle flowmay induce melting structures not only in the arc but also in the back-arc environments (Conder et al., 2002).”
Rayleigh^Taylor instabilities from hydration and melting propel 'cold plumes' at subduction zones (2003, background): “Thus, the rising of cold plumes is accelerated by the feedback from progressive melting caused by shear and conductive heating and decompression [11,55].”