Мақаланы E-mail арқылы жіберу Microphase Heterogenization of High-Iron Bauxite as a Result of Thermal Radiation
- Авторлар: 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
-
Мекемелер:
- Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch
- Chinakal Institute of Mining, Siberian Branch
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Шығарылым: Том 55, № 5 (2019)
- Беттер: 811-823
- Бөлім: Mineral Dressing
- URL: https://ogarev-online.ru/1062-7391/article/view/184762
- DOI: https://doi.org/10.1134/S1062739119056185
- ID: 184762
Дәйексөз келтіру
Ашық рұқсат
Рұқсат берілді
Тек жазылушылар үшін
Аннотация
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.
Авторлар туралы
I. Razmyslov
Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch
Хат алмасуға жауапты Автор.
Email: razmyslov-i@mail.ru
Ресей, Syktyvkar, 167982
O. Kotova
Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch
Email: kondr@misd.ru
Ресей, Syktyvkar, 167982
V. Silaev
Yushkin Institute of Geology and Mineralogy, Komi Science Center, Ural Branch
Email: kondr@misd.ru
Ресей, Syktyvkar, 167982
V. Rostovtsev
Chinakal Institute of Mining, Siberian Branch
Email: kondr@misd.ru
Ресей, Novosibirsk, 630091
D. Kiseleva
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Хат алмасуға жауапты Автор.
Email: podarenka@mail.ru
Ресей, Yekaterinburg, 620016
S. Kondrat’ev
Chinakal Institute of Mining, Siberian Branch
Хат алмасуға жауапты Автор.
Email: kondr@misd.ru
Ресей, Novosibirsk, 630091
Қосымша файлдар
