Critical metals in manganese nodules from the Cook Islands EEZ, abundances and distributions

被引:127
作者
Hein, James R. [1 ]
Spinardi, Francesca [1 ]
Okamoto, Nobuyuki [2 ]
Mizell, Kira [1 ]
Thorburn, Darryl [3 ]
Tawake, Akuila [4 ]
机构
[1] US Geol Survey, PCMSC, Santa Cruz, CA 95060 USA
[2] JOGMEC, Met Min Technol Dept, Sea Floor Mineral Resources R&D Div, Minato Ku, Tokyo 1050001, Japan
[3] Seabed Minerals Author, Avarua, Rarotonga, Cook Islands
[4] SPC, SOPAC Div, Suva, Fiji
关键词
Manganese nodules; Cook Islands EEZ; Critical metals; Mn; Ti; Co; Ni; REY; FERROMANGANESE CRUSTS; SOUTH-PACIFIC; RARE-EARTH; ELEMENTS; COBALT;
D O I
10.1016/j.oregeorev.2014.12.011
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The Cook Islands (Cis) Exclusive Economic Zone (EEZ) encompasses 1,977,000 km(2) and includes the Penrhyn and Samoa basins abyssal plains where manganese nodules flourish due to the availability of prolific nucleus material, slow sedimentation rates, and strong bottom currents. A group of CIs nodules was analyzed for mineralogical and chemical composition, which include many critical metals not before analyzed for CIs nodules. These nodules have varying sizes and nuclei material; however all are composed predominantly of delta-MnO2 and X-ray amorphous iron oxyhydroxide. The mineralogy, Fe/Mn ratios, rare earth element contents, and slow growth rates (mean 1.9 mm/10(6) years) reflect formation primarily by hydrogenetic precipitation. The paucity of diagenetic input can be explained by low primary productivity at the surface and resultant low organic matter content in seafloor sediment, producing oxic seafloor and sub-seafloor environments. The nodules contain high mean contents of Co (0.41%), Ni (0.38%), Ti (1.20%), and total rare earth elements plus yttrium (REV; 0.167%), and also high contents of Mo, Nb, V, W, and Zr. Compiled data from a series of four cruises by the Japan International Cooperation Agency and the Mining agency of Japan from 1985 to 2000 were used to generate a map that defines the statistical distribution of nodule abundance throughout the EEZ, except the Manihiki Plateau. The abundance distribution map shows a belt of high nodule abundance (19-45 kg/m(2)) that starts in the southeast corner of the EEZ, runs northwest, and also bifurcates into a SW trending branch. Small, isolated areas contain abundances of nodules of up to 58 kg/m(2). Six similar to 20,000 km(2) areas of particularly high abundance were chosen to represent potential exploration areas, and maps for metal concentration were generated to visualize metal distribution and to extrapolate estimated metal tonnages within the six sites and the EEZ as a whole. Grades for Mn, Cu, and Ni are low in Cis nodules in areas of high abundance; however, Ti, Co, and REY show high contents where nodule abundances are high. Of the six areas identified to represent a range of metal contents, one at the northern end of the N-S abundance main belt optimizes the most metals and would yield the highest dry metric tons for Mn (61,002,292), Ni (1,247,834), Mo (186,166), V (356,247), W (30,215), and Zr (195,323). When compared with the Clarion-Clipperton Zone, the Cis nodules show higher nodule abundances (>25 kg/m(2) over similar to 123,844 km(2)), and are more enriched in the green-tech, high-tech, and energy metals Co, Ti, Te, Nb, REY, Pt, and Zr. The CIs EEZ shows a significant resource potential for these critical metals due to their high prices, high demand, and the high nodule abundance, which will allow for a smaller footprint for a 20-year mine site and therefore smaller environmental impact. Published by Elsevier B.V.
引用
收藏
页码:97 / 116
页数:20
相关论文
共 29 条
[1]   ABUNDANCES OF THE ELEMENTS - METEORITIC AND SOLAR [J].
ANDERS, E ;
GREVESSE, N .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (01) :197-214
[2]   Discriminating between different genetic types of marine ferro-manganese crusts and nodules based on rare earth elements and yttrium [J].
Bau, M. ;
Schmidt, K. ;
Koschinsky, A. ;
Hein, J. ;
Kuhn, T. ;
Usui, A. .
CHEMICAL GEOLOGY, 2014, 381 :1-9
[3]  
CLARK AL, 1995, EC DEV POTENTIAL MAN
[4]  
Cronan D. A, 2013, 1 COOK ISL SEAB MIN
[5]  
Cronan D.S., 2006, J MAR SCI ENV, VC4, P41
[6]   An ITRAX Geochemical Study of Ferromanganiferous Sediments from the Penrhyn Basin, South Pacific Ocean [J].
Cronan, David S. ;
Rothwell, Guy ;
Croudace, Ian .
MARINE GEORESOURCES & GEOTECHNOLOGY, 2010, 28 (03) :207-221
[7]   MANGANESE NODULES IN THE EEZS OF ISLAND COUNTRIES IN THE SOUTHWESTERN EQUATORIAL PACIFIC [J].
CRONAN, DS ;
HODKINSON, RA ;
MILLER, S .
MARINE GEOLOGY, 1991, 98 (2-4) :425-435
[8]   DISTRIBUTION OF RARE-EARTH, PRECIOUS METAL AND OTHER TRACE-ELEMENTS IN RECENT AND FOSSIL DEEP-SEA MANGANESE NODULES [J].
GLASBY, GP ;
KEAYS, RR ;
RANKIN, PC .
GEOCHEMICAL JOURNAL, 1978, 12 (04) :229-243
[9]  
Hein J., 2013, Deep Sea Minerals: Manganese Nodules
[10]  
A Physical, Biological, Environmental, and Technical Review, P7