О ПРИРОДЕ «ГОЛУБОВАТОГО МАГНЕТИТА» ИЗ ЖЕЛЕЗИСТЫХ КВАРЦИТОВ КОЛЬСКОГО ПОЛУОСТРОВА
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| dc.contributor.author | Балабонин, Н.Л. | |
| dc.contributor.author | Иванюк, Г.Ю. | |
| dc.date.accessioned | 2022-05-31T06:29:34Z | |
| dc.date.available | 2022-05-31T06:29:34Z | |
| dc.date.issued | 1995 | |
| dc.identifier.citation | Записки РМО, 2017, № 1, С. 84-102 | ru_RU |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/37849 | |
| dc.description.abstract | Small bluish-grey spots are observed very often in polished sections of ordinary brownish-grey magnetite. Study realized on hundreds of samples from the Kola banded iron ore formation (BIF) has shown the presence of both «bluish» and «brownish» magnetites in 30 % of the BIF ores. The «bluish» magnetite has the higher iron grade, comparatively to the brownish phase, and physical properties of magnetites containing one (brownish) or both phases are more diverse than those of magnetites differing by the trace elements content only. | ru_RU |
| dc.language.iso | ru | ru_RU |
| dc.subject | магнетит | ru_RU |
| dc.subject | Кольский полуостров | ru_RU |
| dc.title | О ПРИРОДЕ «ГОЛУБОВАТОГО МАГНЕТИТА» ИЗ ЖЕЛЕЗИСТЫХ КВАРЦИТОВ КОЛЬСКОГО ПОЛУОСТРОВА | ru_RU |
| dc.title.alternative | ON THE NATURE OF «BLUISH» MAGNETITE FROM THE BANDED IRON ORE FORMATION OF KOLA PENINSULA | ru_RU |
| dc.type | Article | ru_RU |
| dc.subject.udc | 553.311.2+549.08.53+550.424 |
