Rare Th–Sc Minerals in Picrites of the Southern Urals and Their Genetic Value


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Abstract

The first data on the discovery of Th–Sc mineralization in the pyritic complexes of the Southern Urals are presented. The minerals of Th (thorite) and Sc-containing thorium minerals are described. The conclusion is made that the Th–Sc mineralization formed due to crystallization of a residual melt in the local volume.

About the authors

S. G. Kovalev

Institute of Geology, Ufa Federal Research Center,
Russian Academy of Sciences

Author for correspondence.
Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077

V. N. Puchkov

Institute of Geology, Ufa Federal Research Center,
Russian Academy of Sciences

Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077

S. S. Kovalev

Institute of Geology, Ufa Federal Research Center,
Russian Academy of Sciences

Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077

S. I. Vysotsky

Institute of Geology, Ufa Federal Research Center,
Russian Academy of Sciences

Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077

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