Devolatilization during subduction
Abstract
Subducted crust refertilizes the subarc mantle wedge as well as the deep convecting mantle. In the subarc region, mass transfer occurs mainly through fluids, melts, or supercritical liquids. Experiments show that devolatilization reactions may occur at almost any depth in the chemically complex subducting lithosphere. Extreme temperature gradients across the slab lithosphere, the subduction channel, and the mantle hanging wall promote...
Paper Details
Title
Devolatilization during subduction
Published Date
Jan 1, 2014
Journal
Volume
4
Pages
669 - 701
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