Value Δ34S  in millerite and genesys of clinochlore-brindleyite-chamosite nickel ores in the Elov supergene deposit (North Urals)

O. P. Mezentseva; I. V. Talovina

Vol 189

Pages:

58-61

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Article

Value Δ34S in millerite and genesys of clinochlore-brindleyite-chamosite nickel ores in the Elov supergene deposit (North Urals)

Authors:

O. P. Mezentseva¹

I. V. Talovina²

About authors

1 — post-graduate student Saint Petersburg State Mining Institute (Technical University)
2 — post-doctoral student Saint Petersburg State Mining Institute (Technical University)

Date submitted:

2010-07-10

Date accepted:

2010-09-24

Date published:

2011-03-21

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.

Value Δ34S in millerite and genesys of clinochlore-brindleyite-chamosite nickel ores in the Elov supergene deposit (North Urals)

Abstract

References

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