NEPHELINE BEARING TYLAITES IN A DUNITE-CLINOPYROXENITE-GABBRO ASSOCIATION FROM THE PLATINUM BEARING BELT OF THE URALS
| dc.contributor.author | Fershtater G.B. | |
| dc.contributor.author | Pushkarev Y.V. | |
| dc.date.accessioned | 2020-11-09T07:48:58Z | |
| dc.date.available | 2020-11-09T07:48:58Z | |
| dc.date.issued | 1992 | |
| dc.description.abstract | Tylaites - feldspathic olivine clinopyroxenites from the Tagil'skiy dunite-clinopyroxenite massif in the platinum-bearing belt of the Urals - are of magmatic origin. They are composed of phenocrysts of zonal clinopyroxene, cemented by a fine-grained aggregate of olivine, clinopyroxene, biotite and magnetite, and also orthoclase-plagioclase and orthoclase-nepheline (pseudoleucitic) symplektites. The rocks represent hypabyssal facies of olivine clinopyroxenites, which indicates that the dunite-clinopyroxenite-gabbro formation in the platinum-bearing belt of the Urals belongs to a volcano-plutonic association. | |
| dc.identifier | https://elibrary.ru/item.asp?id=38602280 | |
| dc.identifier.citation | Известия Российской академии наук. Серия геологическая, 1992, , 4, 74-84 | |
| dc.identifier.issn | 0321-1703 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/18758 | |
| dc.title | NEPHELINE BEARING TYLAITES IN A DUNITE-CLINOPYROXENITE-GABBRO ASSOCIATION FROM THE PLATINUM BEARING BELT OF THE URALS | |
| dc.type | Статья |