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Karelia ( Karelian and Finnish: Karjala [ˈkɑrjɑlɑ]; Russian: Каре́лия, romanized : Kareliya [kɐˈrʲelʲɪjə], historically Коре́ла, Korela [ kɐˈrʲelʲə ]; Swedish: Karelen [kɑˈreːlen]) is an area in Northern Europe of historical significance for Russia (including the Soviet era), Finland, and Sweden.
May 1, 2015 · The Mesoarchean Kola-Karelia continent in the eastern Fennoscandian Shield includes three tectonic provinces, Kola, Karelia and Belomoria, that were formed by the Paleoarchean and Mesoarchean microcontinents.
- Michael V. Mints, Ksenia A. Dokukina, Ksenia A. Dokukina, Alexander N. Konilov, Tatiana V. Kaulina, ...
- 2015
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Sep 15, 1986 · The Karelian craton (> 2.3 Ga) has been recognized within the Baltic Shield. The basement of the eraton is a late Archaean granite--greenstone terrain. The greenstone belts from different regions of Karelia show variations in age and composition of volcanic rocks.
- S.B. Lobach-Zhuchenko, O.A. Levchenkov, V.P. Chekulaev, I.N. Krylov
- 1986
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Apr 8, 2020 · The age coincides with major deformation and metamorphism in the Karelia Province around 1.76 Ga. Zircon from the Jänesselkä mafic-ultramafic complex yields a minimum age of 2425±17 Ma, complying...
Jul 1, 2015 · ABSTRACT The Mesoarchean Kola-Karelia continent in the eastern Fennoscandian Shield includes three tectonic provinces, Kola, Karelia and Belomoria, that were formed by the Paleoarchean and...
Jan 1, 1997 · The Karelian granite–greenstone terrain is typified by the extensive development of Late Archaean (Lopian) greenstone belts, which represent the relicts of elongate zones preserved after Late Archaean granite formation, metamorphism, and folding events.
