Feeding andesitic eruptions with a high-speed connection from the mantle

Philipp Ruprecht () and Terry Plank
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Philipp Ruprecht: Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W
Terry Plank: Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W

Nature, 2013, vol. 500, issue 7460, 68-72

Abstract: Diffusion modelling of nickel in mantle melts beneath a volcano reveals the short timescales of magma movement from the base of the crust to the surface in the months to years before an eruption.

Date: 2013
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DOI: 10.1038/nature12342

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