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In situ oxygen isotope analysis of garnet from high pressure metamorphic veins of the Italian Western Alps and New Caledonia: Resolving fluid flow regimes in subducted crust

S. A. Groflin, Carl J. Spandler, John Cliff

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Key concepts: Geology, Metamorphic rock, Crust, Subduction, Isotopes of oxygen, Geochemistry, Oceanic crust, Seismology

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In situ oxygen isotope analysis of garnet from high pressure metamorphic veins of the Italian Western Alps and New Caledonia: Resolving fluid flow regimes in subducted crust — Research Paper | ScholarLens