Value Δ34S in millerite and genesys of clinochlore-brindleyite-chamosite nickel ores in the Elov supergene deposit (North Urals)
About authors
- 1 — Saint Petersburg State Mining Institute (Technical University)
- 2 — 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 34 S/ 32 S 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.
References
- Вторушин А.В. Мезозойские железные руды Серовского района / А.В.Вторушин, Н.А.Журавлева. М., 1967. 166 с.
- Кононова Л.И. Серовское месторождение гипергенного никеля / Л.И.Кононова, К.Г.Бородина, Н.Д.Вохмятина // Рудоносные коры выветривания. М.: Наука, 1974. С.163-172.
- Костов И. Минералогия. М., 1971. 585 с.
- Михайлов Б.М. Перспективы развития сырьевой базы никелевой промышленности Урала // Региональная геология и металлогения. 2002. № 15. С. 97-109.
- Хефс Й. Геохимия стабильных изотопов. М.: Мир, 1983. 200 с.
Similar articles
Simulation of swinging movement autoresonant electric drive with nonsymmetric excitation
2011 A. N. Fomenko
The autoresonant asynchronous electric drive of dynamically counterbalanced drilling string on carrying cable with swinging movement fluctuations amplitude stabilization
2011 E. A. Zagrivnyi, V. V. Ivanik
Methodology of rehabilitation move plants, animals in the development of draft comprehensive development area and its economic assessment
2011 A. O. Kharchenko