Genesis of augite-garnet rocks based on new data
Abstract
The structure of parts of the earth’s crust, such as the modern Ural Range is something so immensely complex that no human imagination is able to comprehend it in all its details, and any attempt in this direction reduces it to a more or less detailed schematic representation. But especially grandiose mining areas conceal not only this complexity of structure, but also so many subsequent alterations and transformations that even a schematic representation of the processes that occurred there encounters barely surmountable difficulties. It is enough to point to the intense activity of metamorphism and weathering to highlight these distinctive features. See the results of the study in the article.
None
References
- E. D. Stratanovich. On the Question of the Origin of Iron and Copper Ores. Gornyi Zhurnal, 1903.
- E. S. Fedorov. Kedabekite and Violaite. Izvestiya Moskovskogo Sel'skokhozyaistvennogo Instituta (Annales de l'Institut Agronomique de Moscou), 1901.
- E. S. Fedorov. The Rocks of Kedabek' in Zapiski Imperatorskoi Akademii Nauk (Notes of the Imperial Academy of Sciences), vol. XIV, no. 3.