Original paper
Arc magmas oxidized by water dissociation and hydrogen incorporation in orthopyroxene
Abstract
Elevated H2O concentrations and oxygen fugacities are two fundamental properties that distinguish magmas formed in subduction zones from new crust generated at mid-ocean ridges. However, the mechanism of magma oxidation and how it relates to the increase in H2O remain unclear. In this study, we used infrared spectroscopy of mantle wedge orthopyroxene to trace the temporal and spatial evolution of oxygen fugacity during the transport of hydrous...
Paper Details
Title
Arc magmas oxidized by water dissociation and hydrogen incorporation in orthopyroxene
Published Date
Jul 29, 2019
Journal
Volume
12
Issue
8
Pages
667 - 671
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Notes
History