Argon, oxygen, and boron isotopic evidence documenting 40 Ar E accumulation in phengite during water-rich high-pressure subduction metasomatism of continental crust
Argon, oxygen, and boron isotopic evidence documenting 40 Ar E accumulation in phengite during water-rich high-pressure subduction metasomatism of continental crust
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Keywords
Ar/, Ar, high-pressure, excess , Ar, phengite/fluid partition coefficient for Ar
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