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The First Find of Visible Gold in Ferromanganese Crusts of the Pacific Ocean

机译:太平洋铁锰结壳中可见金的首次发现

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摘要

Gold in marine ferromanganese crusts and concretions was registered using an electron microscope. Fe-Mn crusts of seamounts contain native gold as individual particles of elongated-oval shape with a length up to 0.8 μm, as well as on the surface of verna-dite globules and in goethite aggregates with a size of 0.008-0.01 μm [1]. Native gold in concretions of abyssal basins of the Pacific Ocean is represented [2] by round and elongated-oval particles with a size up to 0.5 μmand flakelike aggregates with a size up to 3 μm.
机译:使用电子显微镜对海洋锰铁结壳和混凝土中的金进行记录。海山的铁锰壳中含有天然金,这些金属为长椭圆形的单个颗粒,长度最大为0.8μm,在白云石小球的表面和针铁矿聚集体中的大小为0.008-0.01μm[1 ]。太平洋深渊盆地中的天然金以圆形和细长的椭圆形颗粒表示[2],椭圆形颗粒的大小最大为0.5μm,鳞片状聚集体的最大大小为3μm。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|422-426|共5页
  • 作者单位

    Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, Russia;

    Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, Russia;

    Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, Russia;

    Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, Russia;

    Far East Geological Institute, Far East Branch, Russian Academy of Sciences, Vladivostok, Russia;

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