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The distribution of Fe ions in chlorites.
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| dc.contributor.author | Bakhtin A. | |
| dc.date.accessioned | 2018-09-14T20:09:12Z | |
| dc.date.available | 2018-09-14T20:09:12Z | |
| dc.date.issued | 1986 | |
| dc.identifier.issn | 0016-7029 | |
| dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/132166 | |
| dc.description.abstract | Discusses the distribution of Fe 2+ and Fe 3+ between the brucite and talc layers. Data obtained indicate a clear-cut relationship between the peak position for Fe 2+ and the distribution between the 2 types of layer. The distribution of Fe 3+ is controlled by the size of the octathedra in the layers. -A.Hall | |
| dc.relation.ispartofseries | Geochemistry International | |
| dc.title | The distribution of Fe ions in chlorites. | |
| dc.relation.ispartofseries-issue | 4 | |
| dc.relation.ispartofseries-volume | 23 | |
| dc.collection | Публикации сотрудников КФУ | |
| dc.relation.startpage | 63 | |
| dc.source.id | SCOPUS00167029-1986-23-4-SID0022845166 |
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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.