CRYSTAL CHEMISTRY OF CR-SPINEL FROM THE IMANDRA LAYERED PLUTON, KOLA PENINSULA
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Zaitseva T.S. | |
dc.contributor.author | Goncharov G.N. | |
dc.contributor.author | Gittsovich V.N. | |
dc.contributor.author | Semenov V.G. | |
dc.date.accessioned | 2021-02-25T05:13:22Z | |
dc.date.available | 2021-02-25T05:13:22Z | |
dc.date.issued | 2001 | |
dc.identifier | https://elibrary.ru/item.asp?id=13385851 | |
dc.identifier.citation | Geochemistry International, 2001, 39, 5, 479-486 | |
dc.identifier.issn | 0016-7029 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/25715 | |
dc.description.abstract | Cr-spinel from the Imandra layered pluton was studied by a variety of methods including mineralogical and petrographic investigations, microprobe, infrared (IR) spectroscopy, XRD, and Mössbauer spectroscopy on 57Fe nuclei. The Imandra Cr-spinel is a multicomponent (Fe2+, Mg)(Cr, Al, Fe3+)2O4 solid solution, which underwent exsolution during cooling after being crystallized to form two major cluster groups composed of chromite and spinel; the domain size was not larger than 6 μm. The concordant variation of chemical compositions in both cluster groups was governed by the equilibrium redistribution of chemical elements according to the occupancy of energetically advantageous cation sites. | |
dc.title | CRYSTAL CHEMISTRY OF CR-SPINEL FROM THE IMANDRA LAYERED PLUTON, KOLA PENINSULA | |
dc.type | Статья |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru