Sm-Nd isotopy of the dykes of the Vorontsovskoe gold-ore deposit (Northern Urals)

descriptionPublicationkeyboard_double_arrow_right Article , Other literature type 01 Jan 2020Publisher:Komi SC UB RASJournal:Vestnik of Geosciences, volume 9, pages 3-6 (issn: 2712-7761,

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Authors: O. B. Azovskova; E. I. Soroka; M. Yu. Rovnushkin; N. G. Soloshenko;

doi: 10.19110/geov.2020.9.1

Sm-Nd isotopy of the dykes of the Vorontsovskoe gold-ore deposit (Northern Urals)

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Abstract

The Vorontsovskoye gold-ore deposit (Northern Urals) generally corresponds to the Carlin-type. One of the deposit features is the presence of numerous dykes of mafic and middle chemical composition, of normal and increased alkalinity. Sm-Nd isotope studies for the first time confirmed the dykes formation age 340 ± 35 Ma. These data can be indicative of the post-collisional stage of magmatism in this area. The positive Nd values suggest a probable abyssal magmatic source of Nd.

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Sm-Nd isotopy of the dykes of the Vorontsovskoe gold-ore deposit (Northern Urals)

Sm-Nd isotopy of the dykes of the Vorontsovskoe gold-ore deposit (Northern Urals)

2 Research products, page 1 of 1

Pokhodyashinite, CuTlSb.sub.2./sub.(Sb.sub.1-x./sub.Tl.sub.x./sub.)AsS.sub.7-x./sub., a new thallium sulfosalt from the Vorontsovskoe gold deposit, Northern Urals, Russia

Isotopic (δ13C, δ18O, Rb-Sr and Sm-Nd) Studies of Carbonates from the Vorontsovskoe Gold Deposit (Northern Urals)