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Vol 194
Pages:
91-95
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RUS
Article

Row of chemical element mobility In rich lizardite-nepouite ores of the Elov supergene Nickel deposit (Northern Urals)

Authors:
O. P. Mezentseva1
V. G. Lazarenkov2
I. V. Talovina3
N. I. Vorontsova4
About authors
  • 1 — post-graduate student Saint Petersburg State Mining University
  • 2 — Ph.D., Dr.Sci. professor Saint Petersburg State Mining University
  • 3 — Ph.D. associate professor Saint Petersburg State Mining University
  • 4 — Ph.D. assistant lecturer Saint Petersburg State Mining University
Date submitted:
2010-12-03
Date accepted:
2011-02-22
Date published:
2011-12-30

Abstract

We have analysed chemical of nepouites. NiO content in then ranges from 13,00 to 35,18 %, MgO from 18,29 to 44,61 %, i.e. the composition of nepouite corresponds to the composition of Mg-nepouite. General row of chemical element mobility in lizardite – nepouite ores of the Elov supergene nickel deposit is the following: (Mo, Sb, Se, W)20-35 > (Sn, As, Ni)10-20 > (Pb, Be, U)3-7 > (Ti, Ga, Mn)1-3 > (Th, Rb, Si)~1 > (Al, V, Co, Tm, Zn, Mg)0,6-0,9 > (Yb, Ca, Cu)0,4-0,5 > (Sc, Cr, Zr, Sr, Ba, Y, Ta, TR)0,1-0,4 > (Cs, Nb; Ag, Te, Bi, Au)< 0,01-0,1.

Область исследования:
(Archived) Current problems in geology and exploration of mineral deposits
Keywords:
Elov deposit Northern Urals nickel ore nepouite lizardite row of chemical element mobility
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References

  1. Maksimovich Z.M. Isomorphic series of lizarditenepouite // Proceedings of the Mineralogical Society of the USSR. 1973. Vol.102. N 2. P.143-149.
  2. Nickeliferous weathering crust of the Ural. Moscow, 1970. 285 p.
  3. Technologic mineralogy of supergene nickel ores. Leningrad, 1988. 274 p.
  4. Brindley G.W. The structure and chemistry of hydrous nickel-containing silicate and aluminate minerals // Bull. BRGM. Sec.2. 1978. N 3. P.233-245.

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