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首页> 外文期刊>Doklady Earth Sciences >Composition and origin of a K2O-rich granite melt in the Mid-Atlantic Ridge, 13A degrees 34' N: Evidence from the analysis of melt inclusions and minerals of the gabbro-plagiogranite association
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Composition and origin of a K2O-rich granite melt in the Mid-Atlantic Ridge, 13A degrees 34' N: Evidence from the analysis of melt inclusions and minerals of the gabbro-plagiogranite association

机译:大西洋中脊13A度34'N处富含K2O的花岗岩熔体的组成和起源:来自辉长辉长岩-斜长花岗岩结合体的熔体包裹体和矿物分析的证据

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  • 来源
    《Doklady Earth Sciences》 |2015年第2期|174-178|共5页
  • 作者单位

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Polar Marine Geosurvey Expedit, St Petersburg, Russia;

    Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia;

    Russian Acad Sci, Physicotechnol Inst, Yaroslavl Branch, Yaroslavl, Russia;

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