摘要
Major and trace elements as well as Pb isotope geochemistry study on the drill core samples of diabase from the Hardat Tolgoi Pb-Zn minefield were carried out to investigate its petrogenesis and tectonic setting. The results show that the diabase is enriched in LILE and depleted in HFSE, formed in volcanic arc environment, and derived from partial melting of lithospheric mantle with crustal contamination.