Polygenetic and polychronic uranium mineralization at deposits of the Khiagda ore field, Buryatia


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The unique combination of several exogenic processes augmenting uranium mineralization followed one another in time at deposits of the Khiagda ore field and gave rise to the formation of uranium resources exceptional for the paleovalley geologic and economic type. The specific geological evolution, volcanic activity, and regional climatic conditions taken together became the main cause of local occurrence of these deposits.

Sobre autores

B. Kochkin

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Autor responsável pela correspondência
Email: btk@igem.com
Rússia, Moscow, 119017

N. Tarasov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: btk@igem.com
Rússia, Moscow, 119017

O. Andreeva

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: btk@igem.com
Rússia, Moscow, 119017

En. Asadulin

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: btk@igem.com
Rússia, Moscow, 119017

V. Golubev

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: btk@igem.com
Rússia, Moscow, 119017

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