Paleoproterozoic gabbro–diorite–granite magmatism of the Batomga Rise (NE Aldan Shield): Sm–Nd isotope geochemical evidence
- 作者: Kuzmin V.1, Bogomolov E.1,2, Glebovitskii V.2
-
隶属关系:
- Karpinsky Russian Geological Research Institute (VSEGEI)
- Institute of Precambrian Geology and Geochronology
- 期: 卷 466, 编号 2 (2016)
- 页面: 199-205
- 栏目: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/188087
- DOI: https://doi.org/10.1134/S1028334X16020203
- ID: 188087
如何引用文章
详细
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.
作者简介
V. Kuzmin
Karpinsky Russian Geological Research Institute (VSEGEI)
Email: vkkuzmin@mail.ru
俄罗斯联邦, Sredny pr. 74, St. Petersburg, 199106
E. Bogomolov
Karpinsky Russian Geological Research Institute (VSEGEI); Institute of Precambrian Geology and Geochronology
Email: vkkuzmin@mail.ru
俄罗斯联邦, Sredny pr. 74, St. Petersburg, 199106; Makarova nab. 2, St. Petersburg, 199034
V. Glebovitskii
Institute of Precambrian Geology and Geochronology
编辑信件的主要联系方式.
Email: vkkuzmin@mail.ru
俄罗斯联邦, Makarova nab. 2, St. Petersburg, 199034