REGULARITIES OF URANIUM ACCUMULATION EPOCHS IN SEDIMENTARY COVER OF UKRAINIAN SHIELD

Authors

  • E. Sushchuk

Keywords:

Ukrainian Shield, metallogenic epoches, uranium, sedimentary cover, hydrogenic deposits, factors ore- accumulation.

Abstract

History-geological analysis of the Ukrainian Shield sedimentary cover formation allowed discovering the row of ore-controlling factors which have determined the possibility of ore-forming process, its intensity, place and time. There were macrocicles (Yura, Cretaceous, Neocene and Pliocene-Quaternary) in the history of region tectonic development, during which (at certain stages) were created favourable conditions of exogenesis ore-formation (for the different ore-types). Such time-intervals obtained the meaning of metallogenic zones. Regularities of origin of the uranium accumulation epochs in Shield sedimentary cover and the main factors of their formation – climatic, geotectonic, structural, paleogeographic, facial – and also the ore substance source were determined. The productivity of certain epochs was determined; the industrial uranium ore features were characterized. For the Ukrainian Shield territory Early Cretaceous, Late Eocene and Neocene-Quarternary epochs of exogenesis uranium accumulation in sedimentary cover were established. For the first two epochs the syngenetic, diagenetic and exodiagenetic uranium concentrations are characteristic, but they are not industrial because of small scales or low uranium concentrations and unfavorable mining conditions. For industrial uranium ores the Neocene-Quartenary metallogenic epoch is the most productive. The hydrogen ground-infiltrated uranium deposits of this epoch are associated with terrigen coal deposits of Paleocene (mainly Buchaksky Layer of Eocene), which fill up paleo-valleys in crystal basis and which have formed at Neocene-Quarter epoch and continuing to change at this time. Establishment of regularities of the uranium accumulation epochs at the history of sedimentary cover of Ukrainian Shield formation allow to trace the scientific directions and the ways to increase the mineral raw material base of Ukrainian nuclear energy.

References

Кировоградский рудный район. Глубинное строение. Тектонофизический анализ. Месторождения рудных полезных ископаемых. – Киев.- 2013 -500 с.

Металлогения фанерозоя платформенной части Украины / [Гойжевский А.А., Скаржинский В.И., Шумлянский В.А., Сущук Е.Г. и др.] – К.: Наук. думка, 1984. – 202 с.

Генетические типы и закономерности размещения урановых месторождений Украины. – Киев: Наукова думка, 1995. – 396 с.

Шумлянский В.А., Сущук Е.Г. и др. Гидрогенное рудообразование в фанерозое Украины.// Геохимия и экология. – 2003,- вып.8. – С.82-105.

Сущук Е.Г. Закономерности уранонакопления в ходе литогенеза базальных отложений раннего мела на южном склоне Украинского щита.//Збірник наук. праць ІГНС. – 2010. - № 18. – С. 73-79.

Калашник Г.А. Геолого-структурные особенности экзогенно-инфильтрационных месторождений урана в Ингуло-Ингулецком рудном районе Украинского щита.//Наук. Вісник Національного технічного університету. – 2013. - №3. – С.11-18.

Перспективи розвитку уранової сировинної бази ядерної енергетики України. – Киев: Наукова думка, 2014. – 355 с.

Сущук Е.Г. Гидрогенные месторождения урана – природные модели поведения его в зоне гипергенеза. // Зб. Наук. Праць ІГОС НАНУ. – 2008. – вип..16 - С.128-135

Published

2023-06-30