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Oxygen fugacities(    f    O  2)$\left( {{f}_{{{\text{O}}_{2}}}} \right)$   of mantle-derived mafic magmas have important controls on the sulfur status and solubility of the magmas, which are key factors to the formation of magmatic Ni-Cu sulfide deposits, particularly those in convergent margin settings. To investigate thef    O  2${{f}_{{{\text{O}}_{2}}}}$   of mafic magmas related to Ni-Cu sulfide deposits in convergent margin settings, we obtained the magmaf    O  2${{f}_{{{\text{O}}_{2}}}}$   of several Ni-Cu sulfide-bearing mafic-ultramafic intrusions in the Central Asian Orogenic Belt (CAOB), North China, based on the olivine-spinel oxygen barometer and the modeling of V partitioning between olivine and melt. We also calculated the mantlef    O  2${{f}_{{{\text{O}}_{2}}}}$   on the basis of V/ Sc ratios of primary magmas of these intrusions.

american mineralogist

Magma oxygen fugacity of mafic-ultramafic intrusions in convergent margin settings: Insights for the role of magma oxidation states on magmatic Ni-Cu sulfide mineralization