Composition and distribution of REE in ferromanganese crusts of the Belyaevsky and Medvedev seamounts in the Sea of Japan

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• 作者：P. E. Mikhailik (1)
  E. V. Mikhailik (1)
  N. V. Zarubina (1)
  N. N. Barinov (1)
  V. T. S鈥檈din (2)
  E. P. Lelikov (2)
  
• 关键词：ferromanganese crusts ; mineralogy ; geochemistry ; rare ; earth elements ; underwater volcanoes ; Sea of Japan
• 刊名：Russian Journal of Pacific Geology
• 出版年：2014
• 出版时间：September 2014
• 年：2014
• 卷：8
• 期：5
• 页码：315-329
• 全文大小：3,203 KB
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• 作者单位：P. E. Mikhailik (1)
  E. V. Mikhailik (1)
  N. V. Zarubina (1)
  N. N. Barinov (1)
  V. T. S鈥檈din (2)
  E. P. Lelikov (2)
  
  1. Far East Geological Institute, Far East Branch, Russian Academy of Sciences, pr. Stoletiya Vladivostoka 159, Vladivostok, 690022, Russia
  2. Il鈥檌chev Pacific Oceanological Institute, Far East Branch, Russian Academy of Sciences, ul. Baltiiskaya 43, Vladivostok, 690041, Russia
  
• ISSN：1819-7159

文摘

This paper presents the results of the integrated study of ferromanganese crusts from the Belyaevsky (Central Basin) and Medvedev (Honshu Basin) seamounts from the Sea of Japan. The study of the mineral composition using powder diffraction and optical and electron microscopy showed that the crusts are made up of todorokite, birnessite, and pyrolusite minerals typical of hydrothermal ferromanganese deposits of the World Ocean. The composition of the ferromanganese crusts from the Sea of Japan was determined by ICP-MS and ICP-OES. The contents of Mn, Fe, Co, Cu, Ni, and other major and trace elements indicate the hydrothermal genesis of the crusts. The obtained data on the composition of ferromanganese crusts of the Sea of Japan, as well as their comparison with different types of deposits of the World Ocean, suggest the endogenic genesis of the studied crusts. However, the REE and Y distribution patterns testify to a significant admixture of hydrogenic matter, which participated in the growth of ferromanganese crusts from the Belyaevsky and Medvedev seamounts.