Age (U-Pb, SHRIMP-II), Geochemistry of zircon, and conditions of the formation of sapphirine-bearing rocks of the Central Kola granulite-gneiss area-Reference-Cited by-同舟云学术

Age (U-Pb, SHRIMP-II), Geochemistry of zircon, and conditions of the formation of sapphirine-bearing rocks of the Central Kola granulite-gneiss area

Published:2013-11 Issue:1 Volume:453 Page:1121-1126
ISSN:1028-334X
Container-title:Doklady Earth Sciences
language:en
Short-container-title:Dokl. Earth Sc.

Author:

Dolivo-Dobrovol’skii D. V.,Skublov S. G.,Glebovitskii V. A.,Astaf’ev B. Yu.,Voinova O. A.,Shcheglova T. P.

Publisher

Pleiades Publishing Ltd

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)

Link

http://link.springer.com/content/pdf/10.1134/S1028334X13110081.pdf

Reference15 articles.

1. K. Kh. Avakyan, Geology and petrology of the Central Kola Archean granulite-gneiss area (Nauka, Moscow, 1992) [in Russian].

2. L. S. Petrovskaya, F. P. Mitrofanov, T. B. Bayanova, et al., Neoarchean enderbite-granulite complex of the Pulozero-Polnek-Tundra area in the Central Kola Block: stages and thermodynamic regimes of the evolution (Kola Peninsula) (Izd-vo KNTs RAN, Apatity, 2010) [in Russian].

3. T. A. Myskova, N. G. Berezhnaya, V. A. Glebovitskii, et al., Dokl. Earth Sci. 402, 547 (2005).

4. R. G. Berman, Can. Mineral. 29, 833 (1991).

5. R. G. Berman and L. Ya. Aranovich, Contrib. Mineral. Petrol. 126, 1 (1996).

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