ABUNDANCE OF WATER AND TRACE ELEMENTS IN THE ONGONITE MELT OF THE ARY-BULAK MASSIF, EASTERN TRANSBAIKAL REGION: EVIDENCE FROM STUDY OF MELT INCLUSIONS
| dc.contributor.author | Kuznetsov V.A. | |
| dc.contributor.author | Andreeva I.A. | |
| dc.contributor.author | Kovalenko V.I. | |
| dc.contributor.author | Antipin V.S. | |
| dc.contributor.author | Kononkova N.N. | |
| dc.date.accessioned | 2022-07-20T06:12:17Z | |
| dc.date.available | 2022-07-20T06:12:17Z | |
| dc.date.issued | 2004 | |
| dc.description.abstract | The study of melt inclusions in quartz and topaz from ongonites of the Ary-Bulak Massif indicated their formation from the ongonite-type magmatic melt at 650-720°C. The parental magma was significantly enriched in H 2O (5-8.7 wt %), F (6-8 wt %), Li, Rb, Be, As, and W, but depleted in Sr, Ba, and Pb, thus indicating a high degree of differentiation. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=13456441 | |
| dc.identifier.citation | Doklady Earth Sciences, 2004, 396, 4, 571-576 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/38284 | |
| dc.title | ABUNDANCE OF WATER AND TRACE ELEMENTS IN THE ONGONITE MELT OF THE ARY-BULAK MASSIF, EASTERN TRANSBAIKAL REGION: EVIDENCE FROM STUDY OF MELT INCLUSIONS | |
| dc.type | Статья |