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RAS Earth ScienceЛитология и полезные ископаемые Lithology and Mineral Resources

  • ISSN (Print) 0024-497X
  • ISSN (Online) 3034-5375

NEW MINERALOGICAL AND GEOCHEMICAL FEATURES OF THE ORE FERROMANGANESE DEPOSITS OF THE IZU-BONIN AND MARIANA ISLAND ARCS

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PII
S30345375S0024497X25040059-1
DOI
10.7868/S3034537525040059
Publication type
Article
Status
Published
Authors
G.V. Novikov
  • Affiliation: Shirshov Institute of Oceanology of the Russian Academy of Sciences
V. A. Rashidov
  • Affiliation: Institute of Volcanology and Seismology FEB RAS
O.Yu. Bogdanova
  • Affiliation: Shirshov Institute of Oceanology of the Russian Academy of Sciences
Volume/ Edition
Volume / Issue number 4
Pages
435-448
Abstract
Some features of the ferromanganese deposits of the Izu-Bonin and Mariana Island arcs tested in the 1st (1977) and 5th (1978) flights of the R/V Volcanologist are considered. Two types of genetic deposits have been identified - hydrogenic and low-temperature hydrothermal. The main ore minerals of hydrogenic ferromanganese deposits are poorly crystallized structures with a low degree of ordering Fe-vernadite and Mn-feroxygite, with a smaller amount of goethite and bernessite. Low-temperature hydrothermal deposits consist either primarily of bernessite, as well as vernadite and goethite, or of hematite, goethite and feroxygite. Hydrogenic ferromanganese deposits of the Izu-Bonin and Mariana Island arcs are characterized by a Mn/Fe ratio of 0.84-1.36, for low-temperature hydrothermal deposits of the Izu-Bonin arc it is 6.13-13.9. It was found that the content of Co, Ni and Cu is significantly higher in the crusts of the Mariana arc compared with the crusts of the Izu-Bonin arc. The contents of the remaining cations of heavy and rare metals - Pb, Cd, Ba, Sr and others - in the crusts of both arcs are close to each other. The content of most rare earth metal cations in the hydrogenic deposits of the Izu-Bonin and Mariana arcs is comparable to each other. Low-temperature hydrothermal ferromanganese deposits of the Izu-Bonin arc differ significantly from hydrogenic deposits with a low (by 1-2 orders of magnitude) content of cations of non-ferrous, heavy and rare metals. The contents of rare earth metal cations in low-temperature hydrothermal samples of the Izu-Bonin arc are low and range from 0.24 (Tm, Lu) to 32.35 mcg/g (Y). Among all rare earth metal cations, Y, Ce, and Nd are present in the largest amounts in these samples.
Keywords
железомарганцевые отложения Идзу-Бонинская и Марианская островные дуги рудные марганцевые и железистые минералы катионы редкоземельных цветных тяжелых редких металлов
Date of publication
08.12.2025
Year of publication
2025
Number of purchasers
0
Views
30

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