Paleoproterozoic gabbro–diorite–granite magmatism of the Batomga Rise (NE Aldan Shield): Sm–Nd isotope geochemical evidence
- Авторы: Kuzmin V.K.1, Bogomolov E.S.1,2, Glebovitskii V.A.2
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Учреждения:
- Karpinsky Russian Geological Research Institute (VSEGEI)
- Institute of Precambrian Geology and Geochronology
- Выпуск: Том 466, № 2 (2016)
- Страницы: 199-205
- Раздел: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/188087
- DOI: https://doi.org/10.1134/S1028334X16020203
- ID: 188087
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Аннотация
The geochemical similarity and almost simultaneous (2055–2060 Ma) formation of Utakachan gabbro-amphibolite, Jagdakin granodiorite-diorite, Khoyunda granitoid, and Tygymyt leucogranite complexes, which inruded metamorphic formations of the Batomga Group are evidence of their formaton from unified magmatic source. All this makes it possibble to combine aforementioned complexes into the unified Early Proterozoic diferentiated gabbro-diorite-granite complex.
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Об авторах
V. Kuzmin
Karpinsky Russian Geological Research Institute (VSEGEI)
Email: vkkuzmin@mail.ru
Россия, Sredny pr. 74, St. Petersburg, 199106
E. Bogomolov
Karpinsky Russian Geological Research Institute (VSEGEI); Institute of Precambrian Geology and Geochronology
Email: vkkuzmin@mail.ru
Россия, Sredny pr. 74, St. Petersburg, 199106; Makarova nab. 2, St. Petersburg, 199034
V. Glebovitskii
Institute of Precambrian Geology and Geochronology
Автор, ответственный за переписку.
Email: vkkuzmin@mail.ru
Россия, Makarova nab. 2, St. Petersburg, 199034
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