Fast magma ascent, revised estimates from the deglaciation of Iceland
David W. Rees Jones, John F. Rudge

TL;DR
This study revises estimates of magma ascent rates during Iceland's deglaciation, suggesting a maximum steady-state melt velocity of about 30 m/yr, which is faster than traditional microstructural estimates but aligns with geophysical data.
Contribution
The paper introduces a nonlinear, time-dependent model to better estimate steady-state melt velocities, revising previous estimates downward and applying findings to global mid-ocean ridges.
Findings
Maximum steady-state melt velocity in Iceland is about 30 m/yr.
Global melt extraction rates are generally greater than 10 m/yr.
Rapid melt extraction is common at mid-ocean ridges.
Abstract
Partial melting of asthenospheric mantle generates magma that supplies volcanic systems. The timescale of melt extraction from the mantle has been hotly debated. Microstructural measurements of permeability typically suggest relatively slow melt extraction (1 m/yr) whereas geochemical (Uranium-decay series) and geophysical observations suggest much faster melt extraction (100 m/yr). The deglaciation of Iceland triggered additional mantle melting and magma flux at the surface. The rapid response has been used to argue for relatively rapid melt extraction. However, this episode must, at least to some extent, be unrepresentative, because the rates of magma eruption at the surface increased about thirty-fold relative to the steady state. Our goal is to quantify this unrepresentativeness. We develop a one-dimensional, time-dependent and nonlinear (far from steady-state), model forced by the…
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