Year: 2025
Type: article
Abstract: The Bi mineralization is described in quartz-sulfde veins of the Nazarovskoe gold polymetallic deposit (Western Transbaikalia), which is localized within the Eravnino volcano-tectonic structure and is confned to the Nazarovskoe fault zone and the contact with a granodiorite pluton intruding volcanosedimentary rocks. The Bi minerals include Ag-Bi, Cu-Bi, Pb-Bi, and Ag-Pb-Bi sulfosalts, Bi sulfotellurides, aikinite, and native bismuth in assemblage with chalcopyrite and galena. Most Bi minerals are described for the frst time both for the Nazarovskoe deposit and the entire Ozerninsky ore cluster.
Source: МИНЕРАЛОГИЯ (MINERALOGY)
Authors: Yu. Ryzhkova, K. Novoselov, M. Rassomakhin, E. Rozhkov
Institution: Institute of Mineralogy
Language: English
Subfield: Geophysics
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: diamond
OpenAlex ID: W4408842786