Low mantle plume component in 370 Ma old Kola ultrabasic-alkaline-carbonatite complexes: Evidences from rare gas isotopes and related trace elements
| dc.contributor.author | Tolstikhin, I.N. | |
| dc.contributor.author | Kamensky, I.L. | |
| dc.contributor.author | Nivin, V.A. | |
| dc.contributor.author | Vetrin, V.R. | |
| dc.date.accessioned | 2021-10-21T06:31:15Z | |
| dc.date.available | 2021-10-21T06:31:15Z | |
| dc.date.issued | 1998 | |
| dc.description.abstract | During Devonian pulse of alkaline magmatism (370 Ma ago) 18 ultrabasic-alkaline-carbonatite comlexes were formed on the Kola Peninsula. | ru_RU |
| dc.identifier.citation | RUSSIAN JOURNAL OF EARTH SCIENCES, 1998, VOL. 1, NO. 2, p. 179–222 | ru_RU |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/30843 | |
| dc.language.iso | en | ru_RU |
| dc.subject.age | Paleozoic::Devonian | |
| dc.subject.age | Палеозой::Девонская | ru |
| dc.title | Low mantle plume component in 370 Ma old Kola ultrabasic-alkaline-carbonatite complexes: Evidences from rare gas isotopes and related trace elements | ru_RU |
| dc.type | Article | ru_RU |