minerals Article Geochemical Features and Mineral Associations of Differentiated Rocks of the Norilsk 1 Intrusion Nadezhda Tolstykh 1,2,*, Gennadiy Shvedov 3, Aleksandr Polonyankin 4 and Vladimir Korolyuk 1 1 VS Sobolev Institute of Geology and Mineralogy of Siberian Branch of Russian Academy of Sciences, Koptyuga Prospect., 3, 630090 Novosibirsk, Russia;
[email protected] 2 Department of Geology and Geophysics, Novosibirsk State University, Pirogova Ave., 2, 630090 Novosibirsk, Russia 3 Institute of Mining, Geology and Geotechnology, Siberian Federal University, 95 Ave. Prospekt im. Gazety “Krasnoyarskiy Rabochiy”, 660025 Krasnoyarsk, Russia;
[email protected] 4 Russian Platinum LLC, Sivtsev Vrahzek Side-Street, 39, 119002 Moscow, Russia;
[email protected] * Correspondence:
[email protected] Received: 30 June 2020; Accepted: 30 July 2020; Published: 31 July 2020 Abstract: The purpose of this study is to show the patterns of distribution of disseminated sulfide in layered rocks based on the numerous geochemical and mineralogical data obtained for eight boreholes of the Norilsk intrusion (southern part of the Norilsk 1 deposit). There is a common trend of sulfide liquid fractionation in the Main Ore Horizon, which is composed of picritic and taxite (or olivine) gabbro-dolerites: the Ni/Cu in both rock types decreases down all sections, indicating an increase in the degree of fractionation of the sulfide liquid from top to bottom. On the contrary, the Ni/Fe ratios in pentlandite increase in this direction due to an increase in sulfur fugacity. However, picrite and taxite/olivine gabbro-dolerites are very distinctly separated by Ni/Cu values: these values are >1 in picritic gabbro-dolerite while they are always <1 in taxite/olivine gabbro-dolerite.