Uranium isotope fractionation during slab dehydration beneath the Izu arc

Volume: 522, Pages: 244 - 254
Published: Sep 1, 2019
Abstract
Fluids released from subducted slabs impart characteristic geochemical signatures on volcanic arc magmas and residual slabs transported into the deeper mantle. Yet, the sources and transport mechanisms of trace elements released from the slab are speculative. We investigate fluids released from subducted slabs from the perspective of 238U/235U and radiogenic Pb isotope ratios in lavas from the Izu volcanic arc in the Pacific ocean. Izu arc lavas...
Paper Details
Title
Uranium isotope fractionation during slab dehydration beneath the Izu arc
Published Date
Sep 1, 2019
Volume
522
Pages
244 - 254
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