Svecofennian Orogen of the Fennoscandian Shield: Compositional and isotopic zoning and its tectonic interpretation

Author:

Baltybaev Sh. K.

Publisher

Pleiades Publishing Ltd

Subject

Geology

Reference68 articles.

1. Sh. K. Baltybaev and O. A. Levchenkov, “Volcanics in Svecofennides of the Ladoga region and results of U-Pb and Pb-Pb dating of rocks and minerals as a basis for correlation of Svecofennian Events”, Stratigr. Geol. Correlation 13 (2), 119–133 (2005).

2. Sh. K. Baltybaev, V. A. Glebovitsky, I. V. Kozyreva, et al., “The Meyeri Thrust: the main element of the suture at the boundary between the Karelian Craton and the Svecofennian Belt in the Ladoga region of the Baltic Shield”, Dokl. Earth Sci. 348 (4), 581–584 (1996).

3. Sh. K. Baltybaev, V. A. Glebovitsky, I. V. Kozyreva, et al., Geology and Petrology of Svecofennides in the Ladoga Region (St. Petersburg State Univ., St. Petersburg, 2000) [in Russian].

4. Sh. K. Baltybaev, O. A. Levchenkov, L. K. Levsky, et al., “Two metamorphic stages in the Svecofennian domain: Evidence from the isotopic geochronological study of the Ladoga and Sulkava metamorphic complexes”, Petrology 14 (3), 247–261 (2006).

5. Sh. K. Baltybaev, O. A. Levchenkov, and L. K. Levsky, Svecofennides of Fennoscandia: Spatiotemporal Correlation of Paleoproterozoic Processes (Nauka, St. Petersburg, 2009) [in Russian].

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