Minerals Report - International Seabed Authority

Minerals Report - International Seabed Authority Minerals Report - International Seabed Authority

05.02.2013 Views

CHAPTER 3 REGIONAL AND LOCAL VARIABILITY IN THE SPATIAL DISTRIBUTION OF COBALT-BEARING FERROMANGANESE CRUSTS IN THE WORLD’S OCEAN V.M. Yubko, M.E. Melnikov State Scientific Centre, Yuzhmorgeologiya Russian Federation Y. B. Kazmin, A.I. Glumov Ministry of Natural Resources of the Russian Federation The study of cobalt-bearing ferromanganese crusts, one type of mineral resource of the World Ocean seabed, and the possibility of their commercial exploitation, has reached such a stage that there are grounds to address the problem of their exploration and further exploitation not only theoretically, but practically. Modern knowledge of this type of mineral resource was substantiated by the results of specialized research work that has been actively carried out since the end of the 1970s by various scientific and commercial companies from France, Germany, Japan, Russia and the United States. The high level of existing knowledge helps not only to characterize the extent of these crusts, but to validate criteria for prediction and exploration of cobalt-bearing crust fields, and in some cases, to assess their economic significance. The first Russian studies concerning cobalt-bearing ferromanganese crusts were carried out on separate guyots of the Marcus-Necker Ridge (the Mid-Pacific Mountains) of the Central Pacific Ocean in 1968, and in 1970 during the 43 rd and 48 th cruises of RV “Vitiaz” of the Russian Academy of Sciences. Later, as a result of 30 sea cruises of the Academy of Sciences and the Ministry of Natural Resources that were carried out in different regions of the World Oceans much data were obtained about the extent, bedding and features of the structure and composition of ferromanganese crusts which evolved on submarine mountains and uplifts. INTERNATIONAL SEABED AUTHORITY 162

Recently, all the acquired and available published data were systematized and a multi-tier graphical database on cobalt-bearing ferromanganese crusts on the ocean floor was created. Currently the database contains parameters on ore abundance from 20 ore provinces and 64 regions where crusts deposits are located This database is based on information obtained from 2217 sample stations (Figure 1). The digital tiers of the database represent different kinds of maps (bathymetric, geological, metallogenic, etc.) of deposits for the different regions of the oceans, based on the size of the deposits. Five classes are distinguished. INTERNATIONAL SEABED AUTHORITY 163

CHAPTER 3<br />

REGIONAL AND LOCAL VARIABILITY IN THE SPATIAL<br />

DISTRIBUTION OF COBALT-BEARING FERROMANGANESE CRUSTS<br />

IN THE WORLD’S OCEAN<br />

V.M. Yubko, M.E. Melnikov<br />

State Scientific Centre, Yuzhmorgeologiya<br />

Russian Federation<br />

Y. B. Kazmin, A.I. Glumov<br />

Ministry of Natural Resources of the Russian Federation<br />

The study of cobalt-bearing ferromanganese crusts, one type of<br />

mineral resource of the World Ocean seabed, and the possibility of their<br />

commercial exploitation, has reached such a stage that there are grounds to<br />

address the problem of their exploration and further exploitation not only<br />

theoretically, but practically. Modern knowledge of this type of mineral<br />

resource was substantiated by the results of specialized research work that<br />

has been actively carried out since the end of the 1970s by various scientific<br />

and commercial companies from France, Germany, Japan, Russia and the<br />

United States. The high level of existing knowledge helps not only to<br />

characterize the extent of these crusts, but to validate criteria for prediction<br />

and exploration of cobalt-bearing crust fields, and in some cases, to assess<br />

their economic significance.<br />

The first Russian studies concerning cobalt-bearing ferromanganese<br />

crusts were carried out on separate guyots of the Marcus-Necker Ridge (the<br />

Mid-Pacific Mountains) of the Central Pacific Ocean in 1968, and in 1970<br />

during the 43 rd and 48 th cruises of RV “Vitiaz” of the Russian Academy of<br />

Sciences. Later, as a result of 30 sea cruises of the Academy of Sciences and<br />

the Ministry of Natural Resources that were carried out in different regions of<br />

the World Oceans much data were obtained about the extent, bedding and<br />

features of the structure and composition of ferromanganese crusts which<br />

evolved on submarine mountains and uplifts.<br />

INTERNATIONAL SEABED AUTHORITY 162

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!