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The Composition of Ferromanganese Crusts from the Atlantic Ocean

机译:大西洋铁锰铁结壳的组成

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摘要

The ferromanganese crusts (FMC) formed on the surface of many underground mountains and hills are distributed in all oceans, but they have studied insufficiently so far, as studies were focused mainly on the crusts from the Pacific, which are highly enriched in nonferrous metals. Meanwhile, crusts from the Atlantic Ocean are also of interest, especially after the discovery of significant deposits of crust ores on the Knipovich Ridge in the Atlantic Ocean, which have been described previously in several publications [1-15], but their mineral and chemical compositions need further detailed study.
机译:在许多地下山脉和丘陵表面形成的锰铁结壳(FMC)分布在所有海洋中,但是到目前为止,它们的研究不足,因为研究主要集中在太平洋地区的结壳中,该结壳富含有色金属。同时,来自大西洋的地壳也引起人们的兴趣,尤其是在大西洋的Knipovich脊上发现了大量的地壳矿床之后,先前在几篇出版物中已有描述[1-15],但它们的矿物和化学成分成分需要进一步详细研究。

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  • 来源
    《Doklady Earth Sciences》 |2010年第2期|p.1006-1011|共6页
  • 作者

    G. N. Baturin; V. T. Dubinchuk;

  • 作者单位

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii prosp. 36, Moscow, 117997 Russia;

    rnShirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii prosp. 36, Moscow, 117997 Russia;

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