Submit an Article
Become a reviewer
N. I. Vorontsova, I. V. Talovina, V. G. Lazarenkov, A. M. Gaifutdinova, M. Tikhomirova Isotope ratio 87Sr/86Sr in rocks and ores of the Sakhara and Ufalei supergene nickel deposits in Urals. Journal of Mining Institute. Vol 200. p. 179.

Isotope ratio 87Sr/86Sr in rocks and ores of the Sakhara and Ufalei supergene nickel deposits in Urals

Authors:
N. I. Vorontsova I. V. Talovina V. G. Lazarenkov A. M. Gaifutdinova M. Tikhomirova
Date submitted:
2016-11-10
Date published:

Abstract

Isotope ratio 87Sr/86Sr was determined for the first time for the Ufalei and Sakhara supergene nickel deposits. The average obtained 87Sr/86Sr ratio in the Sakhara deposit (0,70838) is higher then in the Ufalei deposit (0,70697). In both deposits 87Sr/86Sr ratio increases from low-altered serpentinite rocks of the lower part of the deposits (0,70583 and 0,70687) to exogenous iron-oxide rocks of the upper part of the deposits (0,70917 and 0,71004).

Similar articles

Go to volume
Identification of ore association by variation of geochemical spectrum of ore-forming elements оn the example of Zolotoe deposit (Yenisei ridge)
A. L. Popov
Experience of the complex application оf geophysical and geoelectrochemical methods for the prediction and prospecting оf mineral deposits
S. G. Alekseev, S. A. Veshev, N. A. Voroshilov
The effect of integration robust regression analysis with inversion of transients for median gradient method at study of diatremes on Anabar shield
Yu. A. Davydenko, A. Yu. Davydenko, I. S. Kupriyanov, P. A. Popkov, S. V. Sleptsov, I. Yu. Pesterev, S. V. Yakovlev