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

I. N. Razmyslov; O. B. Kotova; V. I. Silaev; V. I. Rostovtsev; D. V. Kiseleva; S. A. Kondrat’ev

doi:10.1134/S1062739119056185

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

作者: Razmyslov I.N.¹, Kotova O.B.¹, Silaev V.I.¹, Rostovtsev V.I.², Kiseleva D.V.³, Kondrat’ev S.A.²
隶属关系:
1. Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch
2. Chinakal Institute of Mining, Siberian Branch
3. Zavaritsky Institute of Geology and Geochemistry, Ural Branch
期: 卷 55, 编号 5 (2019)
页面: 811-823
栏目: Mineral Dressing
URL: https://journals.rcsi.science/1062-7391/article/view/184762
DOI: https://doi.org/10.1134/S1062739119056185
ID: 184762

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详细

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.