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

B. T. Kochkin; N. N. Tarasov; O. V. Andreeva; En. E. Asadulin; V. N. Golubev

doi:10.1134/S1075701517020015

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

Authors: Kochkin B.T.¹, Tarasov N.N.¹, Andreeva O.V.¹, Asadulin E.E.¹, Golubev V.N.¹
Affiliations:
1. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Issue: Vol 59, No 2 (2017)
Pages: 141-155
Section: Article
URL: https://ogarev-online.ru/1075-7015/article/view/215159
DOI: https://doi.org/10.1134/S1075701517020015
ID: 215159

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Abstract

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.