Stable isotope evidence for magmatic fluid input during large-scale Na-Ca alteration in the Cloncurry Fe oxide Cu-Au district, NW Queensland, Australia

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Magmatic Fluid ◽  
Fe Oxide ◽  
Isotope Evidence

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Stable Isotope ◽  
Crustal Recycling ◽  
Isotope Evidence

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Isotope Evidence

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Isotope Evidence
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