MULTIPLE MAGMA SOURCES FOR THE PERALKALINE GRANITOIDS AND RELATED ROCKS OF THE KHALDZAN BUREGTE GROUP OF MASSIFS, WESTERN MONGOLIA: ISOTOPIC (NEODYMIUM, STRONTIUM, AND OXYGEN) AND GEOCHEMICAL DATA
| dc.contributor.author | Kovalenko V.I. | |
| dc.contributor.author | Yarmolyuk V.V. | |
| dc.contributor.author | Kozlovskii A.M. | |
| dc.contributor.author | Kovach V.P. | |
| dc.contributor.author | Sal'nikova E.B. | |
| dc.contributor.author | Kotov A.B. | |
| dc.contributor.author | Khanchuk A.I. | |
| dc.date.accessioned | 2022-11-03T10:21:04Z | |
| dc.date.available | 2022-11-03T10:21:04Z | |
| dc.date.issued | 2004 | |
| dc.description.abstract | The Khaldzan Buregte group of alkaline massifs was formed during seven intrusive phases and is confined to a large dike belt within Early Caledonian island-arc ophiolite and normal granite cutting the ophiolite. The uranium isotopic composition of the rock of the massif varies from +5 to +9. With respect to the ratio of compatible and incompatible trace element, the source of the alkaline rocks vary from those OIB. A two stage model was propose for the formation of khaldzan Bburgte group of alkaline massifs. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=13451537 | |
| dc.identifier.citation | Petrology, 2004, 12, 6, 497-518 | |
| dc.identifier.issn | 0869-5911 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/39335 | |
| dc.title | MULTIPLE MAGMA SOURCES FOR THE PERALKALINE GRANITOIDS AND RELATED ROCKS OF THE KHALDZAN BUREGTE GROUP OF MASSIFS, WESTERN MONGOLIA: ISOTOPIC (NEODYMIUM, STRONTIUM, AND OXYGEN) AND GEOCHEMICAL DATA | |
| dc.type | Статья |
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