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
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