Melt inclusions in the olivine from the Nantianwan intrusion: Implications for the parental magma of Ni-Cu-(PGE) sulfide-bearing mafic-ultramafic intrusions of the ∼260 Ma Emeishan large igneous province (SW China)
Pb isotopic compositions of melt inclusion of the Nantianwan intrusion were reported. The parental magma of the Nantianwan intrusion has a high-Mg basaltic composition. The intrusion represents the parental magma of sulfide-bearing intrusions in ELIP.