Age boundaries of formation of the Tomtor alkaline-ultramafic pluton: U-Pb and 40Ar/39Ar geochronological studies

被引:0
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作者
N. V. Vladykin
A. B. Kotov
A. S. Borisenko
V. V. Yarmolyuk
N. P. Pokhilenko
E. B. Sal’nikova
A. V. Travin
S. Z. Yakovleva
机构
[1] Russian Academy of Sciences,Vinogradov Institute of Geochemistry, Siberian Branch
[2] Russian Academy of Sciences,Institute of Precambrian Geology and Geochronology
[3] Russian Academy of Sciences,Sobolev Institute of Geology and Mineralogy, Siberian Branch
[4] Russian Academy of Sciences,Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
来源
Doklady Earth Sciences | 2014年 / 454卷
关键词
206Pb; DOKLADY Earth Science; Nepheline; Siberian Platform; Zircon Crystal;
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摘要
This paper presents the results of geochronological studies of the Tomtor alkaline-ultramafic pluton, one of the largest Nb, Y, Sc, and TR deposits. A new scheme of its magmatism is given. The current K-Ar and Rb-Sr ages of different igneous rocks of the Tomtor pluton range from 800 to 250 Ma [Zaitsev et al., 1992; Frolov et al., 2003]. Such dispersion is probably related to the intense carbonatization of the rocks. The U-Pb zircon and 40Ar/39Ar mica ages indicate two stages of the formation of the pluton (700 and 400 Ma), which agrees well with the age of cycles of rift-related tectonogenesis of the Siberian platform.
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页码:7 / 11
页数:4
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