Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Mineralization and Tectonic Implication

Contributes significantly to exploration of Ni-Cu-PGE deposits particularly those within organic beltConstructs the tectonic evolutionary history of the southern CAOB involving the subduction of South Tianshan ocean and subsequent Junggar oceanProposes a mantle plume + post-orogenic extension model for the generation of mafic-ultramafic complexes in southern CAOBIncludes supplementary material: sn.pub/extras