H2O-rich mantle melting near the slab–wedge interface
Abstract
To investigate the first melts of the mantle wedge in subduction zones and their relationship to primitive magmas erupted at arcs, the compositions of low degree melts of hydrous garnet lherzolite have been experimentally determined at 3.2 GPa over the temperature range of 925–1150 °C. Two starting compositions with variable H2O contents were studied; a subduction-enriched peridotite containing 0.61% Na2O, 0.16 K2O% (wt%) with 4.2 wt% H2O added...
Paper Details
Title
H2O-rich mantle melting near the slab–wedge interface
Published Date
Sep 17, 2019
Volume
174
Issue
10
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