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
Funding:
None
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 control algorithm reagent conditions of flotation copper-nickel ores on the basis of оptimizing the ionic parameters
2011 A. M. Kurchukov
Distribution of groups of trace elements elements by types metasomatic rocks and ores in the Elov nickel deposit
2011 O. P. Mezentseva, I. V. Talovina
Application of the gpr method for investigetion of barring condition and outbarring spaces «Оctyabr’skiy» mine
2011 V. V. Glazunov, S. M. Danilev