Abstract：Eight pyrites from the manganese-bearing rock series of the First Member of Neoproterozoic Datangpo Formation are used for Re-Os isotopic dating at Xixibao orefield in Tongren area, Guizhou province. The analyses yield an isochronic age 459±16 Ma, significantly later than the interglacial depositional age of Datangpo Formation (670~635 Ma), which suggest that the Datangpo Formation was probably affected by the tectonic 〖JP〗thermal activity of Late Caledonian. The pyrites also show high Re, low Os abundance, high Re/Os and 187Os/188Os ratio. The initial 187Os/188Os value is 1.02±0.41, significantly higher than the eigenvalue of mantle magma, which indicate the ore-forming materials are mainly derived from the crustal source.
王丹，廖震文，王生伟，蒋小芳，林方成. 贵州铜仁新元古界大塘坡组黄铁矿Re-Os同位素组成及意义[J]. 中国地质调查, 2015, 2(7): 53-57.
WANG Dan， LIAO Zhen-wen， WANG Sheng-wei， JIANG Xiao-fang， LIN Fang-cheng. Re-Os Isotopic Dating of Pyrite from the Neoproterozoic Datangpo Formation#br# in Tongren, Guizhou and Its Geological Significance. , 2015, 2(7): 53-57.
