Using elemental and boron isotopic compositions of tourmaline to trace fluid evolutions of IOCG systems: The worldclass Dahongshan Fe Cu deposit in SW China
Using elemental and boron isotopic compositions of tourmaline to trace fluid evolutions of IOCG systems: The worldclass Dahongshan Fe Cu deposit in SW China
Authors
Keywords
Tourmaline, IOCG deposit, Boron isotope, Fluid evolution, Kangdian region
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