REE Geochemistry and Resource between Co-Rich Crust and Basement in the Pacific Ocean: Based on Magellan Seamount Sample Research

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Abstract:

Using Magellan Seamount samples in the Pacific area to carry out the REE chemical analysis and microscopic descript,this paper analyze the content of REE between the basement rock and co-rich crust, distribution characteristics, distribution pattern.The results show that: the three layers samples contain high value, total quantity is about 1000×10-6, compared with normal deep sea sediments, foraminiferal nuclear shell and sea water content of rare earth elements10 ~ 100 times; Basement and co-rich crust have shown consistent in distrubution mode, REE content is perfectly high, co-rich crust of REE is mainly controlled by overlying seawater on the rock points erosion. volcanic eruption, ocean floor basalt weathering and biological chemical deposition on the formation of the crust also has certain influence. REE as a huge resource is superior to exploit, The comprehensive development and utilization of mineral resources provided good premise, it is possible to createREE resource utilization of the new way.

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2812-2815

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February 2013

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© 2013 Trans Tech Publications Ltd. All Rights Reserved

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[1] S.V. Margolis, R.G. Burns. Pacific deep-sea manganese nodules: Their distribution, composition, and origin[J]. Annual Review of Earth and Planetary Sciences, 1976, 4: 229.

DOI: 10.1146/annurev.ea.04.050176.001305

Google Scholar

[2] G.P. Glasby. The mineralogy of manganese nodules from a range of marine environment[J]. Marine Geology, 1972, 103: 381.

DOI: 10.1016/0025-3227(72)90071-0

Google Scholar

[3] J. WITSHIRE, WEN X Y, YAO D. Ferromanganese crusts near Johnston Islands : Geochemistry, stratigraphy and economic potential [J]. Marine Georesources and Geotechnology, 1999, 17: 257-270.

DOI: 10.1080/106411999273936

Google Scholar

[4] Wang Zhonggang. REE geochemistry [M] . Beijing: Science Press, (1989).

Google Scholar

[5] J.R. HEIN, F. T MANHEIM, SCHWAB W C , et al . Ferromanganese crusts from Necker ridge , Horizon Guyot , S. P. Lee Guyot : Geological considerations[J] . Marine Geology , 1985, 69: 25-54.

DOI: 10.1016/0025-3227(85)90132-x

Google Scholar

[6] HAL HACH P. Process cont rolling the heavy metal distribution in Pacific ferromanganese nodules and crusts [J] . Geol . Rundsch. 1986 , 1 : 235-247.

DOI: 10.1007/bf01770191

Google Scholar

[7] H. STAUDIGEL, S.R. HART. Alteration of basaltic glass : Mech-anisms and significance for t he oceanic crust s2sea water budget[J] . Geochimica et Cosmochimica Acta , 1983 , 47 : 337-350.

DOI: 10.1016/0016-7037(83)90257-0

Google Scholar

[8] J.N. LUDDEN, THOMPSON G. An evaluation of the behavior oft he rare earth element s during t he weathering of sea floor basalt[J] . Eart h and Planetary Letters , 1979 , 43 : 85-92.

DOI: 10.1016/0012-821x(79)90157-2

Google Scholar

[9] Addy, S. Kumar. Rare earth element patterns in manganese nodules and micronodules from northwest Atlant ic[J]. Geochim. Cosmochim. Acta, 1979, 43: 1105-1115.

DOI: 10.1016/0016-7037(79)90097-8

Google Scholar

[10] L.G.M. Bassbecking. Limit s of the natural environment in terms of pH and oxidation -reduction potentials [J] . J . Gel., 1960, 68: 243-284.

Google Scholar

[11] J.R. Hein. Cobal and platinum-rich ferromanganese crusts and associated substrate rocks from the Marshall Islands[J]. Mar. Geol. , 1988, 78: 225-283.

DOI: 10.1016/0025-3227(88)90113-2

Google Scholar

[12] D.Z. Piper. Rare earth element s in ferromanganese nodules and other marine phases [J] . GeoCHIM. ET Cos-mochim. Acta, 1974b, 38: 1007-1022.

DOI: 10.1016/0016-7037(74)90002-7

Google Scholar