Magnesium and boron isotope evidence for the generation of arc magma through serpentinite mélange melting
Peer-Reviewed Publication
Updates every hour. Last Updated: 29-Apr-2025 09:08 ET (29-Apr-2025 13:08 GMT/UTC)
In a recent paper published in National Science Review, a jointed team of scholars from China and UK has made significant progress in understanding the genesis of volcanic rocks in subduction zones. By analyzing the magnesium and boron isotopic compositions of volcanic rocks and forearc serpentinites from the South Sandwich Island arc, a globally representative island arc, the team proposed a novel mechanism for island arc magma formation. Their findings suggest that island arc volcanic rocks can originate from the partial melting of serpentinite-dominated mélanges. This breakthrough significantly advances the understanding of the processes and mechanisms of material recycling in subduction zones.
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