Fields of carbon metasomatism - indicator of ore deposits

Carbonic metasomatites are very interesting subjects in recent years. The carbonic metasomatites were discovered in ore regions of Central Asia and then in Siberia and other regions of Russian Federation. By the present, the carbonic metasomatite have been discovered in ore regions with various hydrothermal mineralization. The carbonic metasomatites are characterized by black color and fine-grained structures. The carbonic metasomatite contains graphite. Graphite is associated with ilmenite, rutile, sulfides of endogenous origin. The carbonic metasomatite contains increased amounts of metals such as V, Ti, Co, Cu, Zn, Pb, Sn, As, W, Au, Re, Ag, Re, Se, and others. Therefore, the somatites are indicators of ore fields.

Авторы
Tomson I.N. 1 , Polyakova O.P. , Alekseev V.Y.
Редакторы
-
Журнал
Издательство
-
Номер выпуска
5
Язык
Русский
Страницы
656-658
Статус
Опубликовано
Подразделение
-
DOI
-
Номер
-
Том
393
Год
2003
Организации
  • 1 Inst. Geol. Rudn. Mestor. Petr., RAN, Moscow, Russian Federation
Ключевые слова
Composition; Mineral exploration; Natural resources exploration; Ore deposit geology; Sampling; Ore deposit indicators; Ore deposits
Дата создания
19.10.2018
Дата изменения
19.10.2018
Постоянная ссылка
https://repository.rudn.ru/ru/records/article/record/10/