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.

Authors
Tomson I.N. 1 , Polyakova O.P. , Alekseev V.Y.
Editors
-
Publisher
-
Number of issue
5
Language
Russian
Pages
656-658
Status
Published
Department
-
DOI
-
Number
-
Volume
393
Year
2003
Organizations
  • 1 Inst. Geol. Rudn. Mestor. Petr., RAN, Moscow, Russian Federation
Keywords
Composition; Mineral exploration; Natural resources exploration; Ore deposit geology; Sampling; Ore deposit indicators; Ore deposits
Date of creation
19.10.2018
Date of change
19.10.2018
Short link
https://repository.rudn.ru/en/records/article/record/10/