Post-folding magmatism (1.85–1.7 Ga) in the eastern part of the Baltic Shield: Correlation of its structural position and evolution of surrounding complexes

Author:

Terekhov E. N.,Baluev A. S.

Publisher

Pleiades Publishing Ltd

Subject

Paleontology,Stratigraphy,Geology

Reference70 articles.

1. Arzamastsev, A.A., Bea, F., Arzamastseva, L.V., and Montero, P., Proterozoic Polyphase Massif Gremyakha-Vyrmes, Kola Peninsula: An example of Mixing Basic and Alkaline Mantle Melts, Petrologiya, 2006, vol. 14, no. 4, pp. 384–414 [Petrology (Proterozoic Gremyakha-Vyrmes Polyphase Massif, Kola Peninsula: An Example of Mixing Basic and Alkaline Mantle Melts), vol. 14, no. 4, pp. 361–389].

2. Arzamastsev, A.A., Fedotov, Zh.A., and Arzamastseva, L.V., Daikovyi magmatizm severo-vostochnoi chasti Baltiiskogo shchita (Dike Magmatism of the Northeastern Baltic Schield), St. Petersburg: Nauka, 2009.

3. Ahall, K.I. and Larson, S.A., Growth-Related 1.85–1.55 Ga Magmatism in the Baltic Shield: a Review Addressing the Tectonic Characteristics of Svecofennian, TIB 1-Related, and Gothian Events, Geologiska Foreningens I, Stockholm: Forhandlinga, 2000, vol. 122, pp. 193–206.

4. Baluev, A.S., Glukhovskii, M.Z., and Moralev, V.M., Tectonic Conditions of Formation of Massifs of Anorthosite-Rapakivi-Granite Formation in the East European and Siberian Platforms, Izv. Vyssh. Uchebn. Zaved., Geol. Razved., 1997, no. 2, pp. 3–15.

5. Baluev, A.S. and Terekhov, E.N., Different-depth Xenoliths from Devonian Intrusions of the Kola Peninsula: Key to Deciphering Paleogeodynamic Settings of Alcaline Magmatism, Dokl. Akad. Nauk, 2006, vol. 406, no. 5, pp. 651–655 [Dokl. Earth Sci. (Different-depth Xenoliths from Devonian Intrusions of the Kola Peninsula: Key to Deciphering Paleogeodynamic Settings of Alcaline Magmatism), vol. 407, no. 1, pp. 167–171].

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