Value Δ34S in millerite and genesys of clinochlore-brindleyite-chamosite nickel ores in the Elov supergene deposit (North Urals)
About authors
- 1 — post-graduate student Saint Petersburg State Mining Institute (Technical University)
- 2 — post-doctoral student Saint Petersburg State Mining Institute (Technical University)
Abstract
The article deals with genesis of chamosite zone in Elov supergene nickel deposit after the example of clinochlore-brindleyite-chamosite nickel ore. According to obtained data, isotope ratio 34S/32S in millerite from these ore type varies from –35,5 to –45,6±0,6 ‰. This value corresponds to sedimentary rocks und testifies surface exogenous genesis of chamosite nickel ores.
Область исследования:
(Archived) Geology and geophsics
Keywords:
Elov deposit
nickel ore
chamosite
nepouite
lizardite
coefficients of accumulation
trace elements
References
- Vtoruschin A.V., Zhuravleva N.A. Mesozoic ferrous ores of Serov region / A.V.Vtoruschin, N.A. Zhuravleva. Мoscow, 1967. 166 c.
- Kononova L.I. Serov deposit supergene nickel / L.I.Kononova, K.G.Borodina, N.D.Vohmyatina // Orebearing weathering crust. Moscow: Nauka, 1974. P.163-172.
- Costov I. Mineralogy. Moscow. 1971. 585 p.
- Mikhailov B.M. Perspective of mineral base of nickel industry in Urals. // Regionalnaya geologiya I metallogeniya. 2002. № 15. p. 97-109.
- Khefs Y. Geochemistry of stable isotopes. Мoscow: Mir. 1983. 200 p.
Similar articles
The depth estimation of 2D conductive isometrical bodies by singular points at the tipper frequency characteristic
2011 E. Yu. Ermolin, O. Ingerov
Features technology of modelling waste bank phosphite by results to laser-scanning survey
2011 M. Yu. Vasiliev
Automated control system for the flotation process of copper-nickel ores
2011 A. M. Kurchukov, V. N. Kordakov
Simulation of swinging movement autoresonant electric drive with nonsymmetric excitation
2011 A. N. Fomenko