Paleoproterozoic alkaline magmatism of the Murmansky neoarchaean craton, Kola peninsula
- 作者: Petrovskiy M.N.1, Petrovskaya L.S.1
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隶属关系:
- Geological Institute, Kola Science Center RAS
- 期: 卷 148, 编号 2 (2019)
- 页面: 1-11
- 栏目: General section
- URL: https://journals.eco-vector.com/0869-6055/article/view/12736
- DOI: https://doi.org/10.30695/zrmo/2019.1482.00
- ID: 12736
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The article represents results of geological, geochronological and isotope-geochemical studies of the alkaline-ultrabasic massif located in the lower reaches of the Iokanga River in the Karelian-Kola Alkaline Province. The alkaline-ultramafic massif is composed of nepheline clinopyroxenites, nepheline gabbroids, malignites, and nepheline syenites. These rocks are of Paleoproterozoic age. The age of crystallization determined for nepheline clinopyroxenites by the 40Ar/39Ar phlogopite method is 1955 ± 10.8 Ma, and Rb-Sr isochron over the entire pool of samples of the intrusive rocks corresponds to an age of 1937 Ma, at ISr = 0.70316. According to their isotope-geochemical Sm-Nd and Rb-Sr characteristics, rocks of the alkaline-ultrabasic massif in the lower reaches of the Iokanga River have the mantle origin, and the source of their melts was apparently a mantle of the BSE type.
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作者简介
M. Petrovskiy
Geological Institute, Kola Science Center RAS
编辑信件的主要联系方式.
Email: petrovskiy@geoksc.apatity.ru
俄罗斯联邦, Apatity
L. Petrovskaya
Geological Institute, Kola Science Center RAS
Email: petrovskiy@geoksc.apatity.ru
俄罗斯联邦, Apatity
参考
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