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首页> 外文期刊>Doklady Earth Sciences >The Paleoproterozoic Fedorov-Pana Layered PGE Complex of the Northeastern Baltic Shield, Arctic Region: New U-Pb (Baddeleyite) and Sm-Nd (Sulfide) Data
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The Paleoproterozoic Fedorov-Pana Layered PGE Complex of the Northeastern Baltic Shield, Arctic Region: New U-Pb (Baddeleyite) and Sm-Nd (Sulfide) Data

机译:北极地区东北波罗的海盾的古元古代Fedorov-Pana层状PGE复合物:新的U-Pb(Baddeleyite)和Sm-Nd(硫化物)数据

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摘要

For the first time zircons have been extracted from gabbro-norite of a lower layered horizon of the West Pana Massif in the Pt-Pd Kievei deposit of the Fedorov-Pana Layered Complex. Those zircons have been used for U-Pb dating along with Sm-Nd age determination on sulfide minerals. The obtained new isotopic data are a U-Pb zircon age of 2500 +/- 4 Ma, while the Sm-Nd (mineral and whole-rock) isochron yielded 2483 +/- 86 Ma. These results correspond to the first phase of the Pt-Pd reef complex formation in the Layered Complex. The Pt-Pd reef formation has been dated by U-Pb baddeleyite and zircon analyses in the East Pana Massif to 2464 +/- 12 Ma. The 2485-2464 Ma time span corresponds to the second phase of the Pt-Pd reef formation in the Fedorov-Pana ore cluster.
机译:首次从Fedorov-Pana层状复合体的Pt-Pd Kievei矿床的西Pana地块下层地平线的辉长岩-白铁矿中提取锆石。这些锆石已用于硫化物矿物的U-Pb测年以及Sm-Nd年龄测定。获得的新同位素数据是锆石年龄为2500 +/- 4 Ma的U-Pb锆石,而Sm-Nd(矿物和全岩)等时线的年龄为2483 +/- 86 Ma。这些结果对应于分层复合物中Pt-Pd礁复合物形成的第一阶段。 Pt-Pd礁的形成已通过东帕纳地块中的U-Pb Baddeleyite和锆石分析确定为2464 +/- 12 Ma。 2485-2464 Ma时间跨度对应于Fedorov-Pana矿团中Pt-Pd礁形成的第二阶段。

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  • 来源
    《Doklady Earth Sciences》 |2017年第1期|1-5|共5页
  • 作者单位

    Russian Acad Sci, Geol Inst, Kola Sci Ctr, Apatity 184209, Russia;

    Russian Acad Sci, Geol Inst, Kola Sci Ctr, Apatity 184209, Russia;

    Russian Acad Sci, Geol Inst, Kola Sci Ctr, Apatity 184209, Russia;

    Russian Acad Sci, Geol Inst, Kola Sci Ctr, Apatity 184209, Russia;

    Russian Acad Sci, Geol Inst, Kola Sci Ctr, Apatity 184209, Russia;

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