Geology of Mineral Deposits of the Ocean

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".

Deadline for manuscript submissions: closed (30 November 2021) | Viewed by 2759

Special Issue Editors


E-Mail Website
Guest Editor
Department of Mineral Deposits Geology, St. Petersburg State University, 199034 St. Petersburg, Russia
Interests: marine geology; marine mineral deposits; hydrothermal processes; seafloor massive sulfides; metalliferous sediments; mineralogy; geochemistry; isotopic geochronology
Special Issues, Collections and Topics in MDPI journals

E-Mail
Guest Editor
Institute for Geology and Mineral Resources of the Ocean (VNIIOkeangeologia), 190121 St. Petersburg, Russia
Interests: ferromanganese crusts; isotopic composition; arctic ocean; geochemistry
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Unlike the several centuries of geological work on the continents, the active study of the geology of the oceans dates back only half a century. However, it can be said that the tectonics, magmatism, sedimentation, and metallogeny of the oceans have revolutionized geological science. The mineral deposits of the oceans rank below the continental ones in diversity, but their resources for several commodities exceed the resources of on-land deposits. However, a number of issues, including the environmental, technological, and legal aspects of the exploitation of oceanic mineral resources, are still in the development stage, which prevent the start of mining in the near future. This time delay allows extensive scientific research to be undertaken. This research should be of both fundamental and applied nature. In this regard, the potential topics for this Special Issue include distribution, geological settings, age, mineralogy and geochemistry of the deposits, the characteristics of host rocks, exploration methods, and modeling processes. Other topics of interest are the so-called critical minerals that are common in deep-ocean mineral deposits, which will be needed for the rapid development of high-tech, green-tech, and energy applications, and comparisons between ocean- and land-based deposits.

Prof. Dr. Georgy A. Cherkashev
Dr. Natalia Konstantinova
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Minerals is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • marine geology
  • marine minerals
  • exploration methods
  • mineralogy
  • geochemistry

Published Papers (1 paper)

Order results
Result details
Select all
Export citation of selected articles as:

Research

22 pages, 4712 KiB  
Article
Gold in Ferromanganese Deposits from the NW Pacific
by Pavel Mikhailik, Evgenii Mikhailik and Vladimir Ivanov
Minerals 2021, 11(9), 979; https://0-doi-org.brum.beds.ac.uk/10.3390/min11090979 - 08 Sep 2021
Cited by 4 | Viewed by 2142
Abstract
Ferromanganese crusts from four different areas of the North-West Pacific Ocean—the Detroit (northern part of the Imperial Ridge) guyot, the Zubov (Marshall Islands) guyot, the “Gummi Bear” seamount (an intraplate volcano near the Krusenstern FZ), and Belyaevsky volcano (the Sea of Japan)—were studied. [...] Read more.
Ferromanganese crusts from four different areas of the North-West Pacific Ocean—the Detroit (northern part of the Imperial Ridge) guyot, the Zubov (Marshall Islands) guyot, the “Gummi Bear” seamount (an intraplate volcano near the Krusenstern FZ), and Belyaevsky volcano (the Sea of Japan)—were studied. Samples from the Detroit and Zubov guyots and the “Gummi Bear” seamount have similar chemical and mineral compositions of hydrogenetic cobalt-rich ferromanganese crusts. Crust from the Sea of Japan seems to reflect a hydrothermal influence. The gold content in most samples from the Detroit guyot was 68 ppb and from the Zubov guyot varied from 180 to 1390 ppb, which is higher than the average for the Pacific crusts (55 ppb). Gold content in two other samples was less than 10 ppb. Based on the electron microscopic studies, aggregation of gold particles with a size of 680 μm were identified in the Detroit guyot crust. The sizes of the Au particles are up to 10–15 μm, which has not been previously noted. Gold particles similar in morphology and size were also found in the Zubov guyot crust, which is located far from the Detroit guyot. The largest particle of gold (≈60 μm), represented by electrum, was found in the clay substrate from the “Gummi Bear” seamount. The lamellar, rudaceous morphology of the gold particles from the Detroit and Zubov guyots reflects their in situ formation, in contrast to the agglutinated, rounded with traces of dragging gold grain found in the substrate of the sample from the “Gummi Bear” seamount. Three-component (Ag-Au-Cu) gold particles were found in the hydrothermal crust from the Belyaevsky underwater volcano. Grains similar in composition were also found in Co-rich crust. The research results show that the gold was probably added to by hydrothermal fluid in the already-formed hydrogenetic ferromanganese crusts during rejuvenated volcanic stages. Biogeochemical processes may have played a major role in the formation of submicron solid-phase gold particles. Full article
(This article belongs to the Special Issue Geology of Mineral Deposits of the Ocean)
Show Figures

Figure 1

Back to TopTop