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    Hydrothermal remobilization of subseafloor sulfide mineralization along mid-ocean ridges contributes to the global oceanic zinc isotopic mass balance
    Geochimica et Cosmochimica Acta (2022)
    Shili LiaoChunhui TaoHanjie WenWeifang YangJia LiuJohn W. JamiesonÁgata Alveirinho DiasChuanwei ZhuJin LiangWei LiTeng DingXiaohu LiHuichao Zhang
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    Keywords:
    Sulfide Minerals
    Seafloor Spreading
    δ34S
    Topics:
    Geochemistry and Elemental Analysis
    Geological and Geochemical Analysis
    earthquake and tectonic studies
    Hydrothermal remobilization of subseafloor sulfide mineralization along mid-ocean ridges contributes to the global oceanic zinc isotopic mass balance
    Geochimica et Cosmochimica Acta (2022)
    Shili LiaoChunhui TaoHanjie WenWeifang YangJia Liu
    Sulfide Minerals
    Seafloor Spreading
    δ34S
    Citations (1)
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    The sulfide minerals from old mafic intrusion rocks from the Kola Peninsula were analyzed on stable sulfur isotopes. These samples were already dated by the Sm-Nd method. These sulfide samples were evaluated upon a geochemical composition by ICP-MS. The sulfide mineral samples were selected from the main ore-bearing rocks of the Monchetundra layered intrusion. The analyzed sulfides formed several generations of mineralization associated with primary and hydrothermal stage of formation of the deposits. Isotopic studies confirm a few consecutive stages of mineralization. These data were compared with the results of Sm-Nd dating of sulfide mineralization. The results of geochemical and geochronological studies indicate a complementarity in the context of determining the mineralization stages.
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