电邮这篇文章 Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)
- 作者: Vasil’ev Y.R.1,2, Gora M.P.1, Kuzmin D.V.1,2
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隶属关系:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- Novosibirsk State University
- 期: 卷 478, 编号 1 (2018)
- 页面: 103-107
- 栏目: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/192019
- DOI: https://doi.org/10.1134/S1028334X18010282
- ID: 192019
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详细
For the Permian–Triassic foidite and meimechite lavas of Polar Siberia, both the whole-rock petrochemistry and geochemistry and that of melt inclusions in olivine phenocrysts from the same rocks have been demonstrated to be similar. In addition, their isotope characteristics imply the possibility of their generation from an abyssal parental melt compositionally resembling a high–Mg alkaline picrite.
作者简介
Yu. Vasil’ev
Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University
编辑信件的主要联系方式.
Email: meimech@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
M. Gora
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: meimech@igm.nsc.ru
俄罗斯联邦, Novosibirsk
D. Kuzmin
Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University
Email: meimech@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
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