Fluid-metasomatized Rocks with Extremely Low Δ26mg Values in Subducted Oceanic Lithosphere: Implications for Mantle Mg Isotope Heterogeneity and the Origin of Low-Δ26mg Magmas
GEOCHIMICA ET COSMOCHIMICA ACTA（2024）
Key words
Mg isotopes,Fluid metasomatism,Serpentinite,Subduction zone,Mantle heterogeneity
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