Microphase Heterogenization of High-Iron Bauxite as a Result of Thermal Radiation


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Abstract

The results of modification of the Middle Timan high-iron bauxite by thermal radiation, including the earlier unknown phenomenon of phase heterogenization—formation of intrinsic minerals by originally endocryptically disseminated noble, nonferrous, rare and rare-earth micro-elements—are presented. It is possible to utilize this phenomenon for the purpose of commercial application of low-grade bauxite, red mud and other difficult ore.

About the authors

I. N. Razmyslov

Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch

Author for correspondence.
Email: razmyslov-i@mail.ru
Russian Federation, Syktyvkar, 167982

O. B. Kotova

Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch

Email: kondr@misd.ru
Russian Federation, Syktyvkar, 167982

V. I. Silaev

Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch

Email: kondr@misd.ru
Russian Federation, Syktyvkar, 167982

V. I. Rostovtsev

Chinakal Institute of Mining, Siberian Branch

Email: kondr@misd.ru
Russian Federation, Novosibirsk, 630091

D. V. Kiseleva

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Author for correspondence.
Email: podarenka@mail.ru
Russian Federation, Yekaterinburg, 620016

S. A. Kondrat’ev

Chinakal Institute of Mining, Siberian Branch

Author for correspondence.
Email: kondr@misd.ru
Russian Federation, Novosibirsk, 630091

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