Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The paper analyses geological position of the Vorontsovskoe gold deposit which is untypical for the Urals folded belt. This deposit is a part of the ore-magmatic system formed in connection with the Auerbakhovsky massif at the North Urals. There are displayed data on mineralogical-geochemical and petrographic characteristics of studied gold-bearing breccias with detail description of their cement. It contains realgar and orpiment, and, in subordinate quantity, Hg-bearing sphalerite, dimorphite, routhierite and minerals of the gruzdevite-aktashite isomorphous series. Obtained data allow to attribute these gold-bearing breccias, with realgar-orpiment cement, to fluid-explosive formations. This is one of numerous evidences to consider ore deposits connected with Auerbakhovsky massif as parts of a uniform ore-magmatic system with distinct lateral zoning.
Язык оригинала | английский |
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Страницы (с-по) | 29-43 |
Число страниц | 15 |
Журнал | Zapiski Rossiiskogo Mineralogicheskogo Obshchestva |
Том | 146 |
Номер выпуска | 1 |
Состояние | Опубликовано - 1 янв 2017 |
ID: 47779201