Row of chemical element mobility In rich lizardite-nepouite ores of the Elov supergene Nickel deposit (Northern Urals)
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
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
Funding:
None
References
- Maksimovich Z.M. Isomorphic series of lizarditenepouite // Proceedings of the Mineralogical Society of the USSR. 1973. Vol.102. N 2. P.143-149.
- Nickeliferous weathering crust of the Ural. Moscow, 1970. 285 p.
- Technologic mineralogy of supergene nickel ores. Leningrad, 1988. 274 p.
- 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.
Similar articles
Complex substantiation of ways to maintenan stability of local development excavations
2011 S. A. Sidorenko, A. A. Sidorenko
Ways of improving the effectiveness of the Russian mineral resources base of scarce minerals reproduction
2011 N. V. Pashkevich, V. S. Khloponina
Methodological approaches to the economic evaluation of anthropological deposits
2011 O. S. Krasnov, V. A. Salikhov