Abstract
The compositions of the tonalite–trondhjemite–granodiorite (TTG) assemblage and volcanic rocks of the Archaean greenstone belts from different domains of the Karelian province of the Baltic Shield are compared. Neoarchean medium felsic volcanic rocks and TTG of the Central Karelian domain drastically differ from analogous Mesoarchean rocks of the neighboring Vodlozero and West Karelian domains in higher Rb, Sr, P, La, and Ce contents and, correspondingly, values of Sr/Y, La/Yb, and La/Sm, and also in a different REE content distribution owing to different rock sources of these domains. This fact is confirmed by differences in the composition and the nature of the REE distribution in the basic and ultrabasic volcanic rocks making up the greenstone belts of these domains. It is established that the average compositions of Mesoarchean TTG rocks and volcanic rocks of the Karelian province differ markedly from those of plagiogranitoids and volcanic rocks of the recent geotectonic environments in high Mg (mg#) and Sr contents. Neoarchean volcanic rocks of Karelia differ from recent island-arc volcanic rocks, but are similar in composition to recent volcanic rocks of the continental arcs. On the basis of the cumulative evidence, the Karelian province of the Baltic Shield was subject to dramatic changes in the crust formation conditions at the beginning of the Neoarchean at the turn of about 2.75–2.78 Ga. These changes led to formation of volcano-sedimentary and plutonic rock complexes, different in composition from Mesoarchean rocks, and specific complexes of intrusive sanukitoids and granites. Changes and variations in the rock composition were related to the mixing of plume sources with continental crust and/or lithospheric mantle material, likely as a result of the combined effect of plumes and plate tectonics. This process resulted in formation of a younger large fragment of the Archean crust such as the Central Karelian domain which factually connected more ancient fragments of the crust and likely contributed to development of the Neoarchean Kenorland Supercontinent.
Similar content being viewed by others
References
Arestova, N.A., The origin of basalts of Archean greenstone belts of the Baltic Shield: sources and geodynamic regimes of formation as evidenced from the geochemical data, Regional. Geol. Metallogen., 2008, no. 36, pp. 5–18.
Arestova, N.A., Chekulaev, V.P., Matveeva, L.V., et al., New age data on the Archean rocks of the Vodlozero domain, Baltic shield, and their significance for geodynamic reconstructions, Dokl. Earth Sci., 2012, vol. 442, no. 1, pp. 1–7.
Arestova, N.A., Chekulaev, V.P., Lobach-Zhuchenko, S.B., and Kucherovskii, G.A., Formation of the Archean crust of the ancient Vodlozero domain (Baltic shield), Stratigr. Geol. Correl., 2015, vol. 23, no. 2, pp. 119–130.
Arndt, N.R., Brusak, G., and Reischmann, T., The oldest continental and oceanic plateaus: geochemistry of basalts and komatiites of the Pilbara Craton, Spec. Pap.—Geol. Soc. Am., 2001, vol. 362, pp. 359–381.
O’Brien, H., Huhma, H., and Sorionen-Ward, P., Petrogenesis of the late Archean Hattu Schist Belt, Ilomantsi, Eastern Finland: geochemistry and Sr, Nd isotopic composition, in Geological Development, Gold Mineralization and Exploration Methods in the Late Archean Hattu Schist Belt, Ilomantsi, Eastern Finland. Geol. Surv. Finland. Spec. Pap., 1993, vol. 17, pp. 147–184.
Chekulaev, V.P., Geology and composition of the Archean TTG and plagiogranites of the Phanerozoic geodynamic settings: similarity and difference, in Mater. nauchn. konf. “Granit-zelenokamennye sistemy arkheya i ikh pozdnie analogi” (Proc. Sci. Conf. “Archean Granite–Greenstone Systems and their Younger Analogues”), Petrozavodsk, 2009, pp. 176–179.
Chekulaev, V.P., Lobach-Zhuchenko, S.B., Arestova, N.A., et al., Archean magmatism at the northwestern margin of the ancient Vodlozero Domain near Lake Oster, Karelia: geology, geochemistry, and petrology, Petrology, 2002, vol. 10, no. 2, pp. 119–145.
Chekulaev, V.P., Arestova, N.A., Kovalenko, A.V., and Slabunov, A.I., Karelian granite–greenstone belt. Central Karelian Domain, in Rannii dokembrii Baltiiskogo shchita (Early Precambrian of the Baltic Shield), Glebovitskii, V.A., Ed., St. Petersburg: Nauka, 2005, pp. 395–0471.
Condie, K.C. and Kröner, A., When did plate tectonics begin? Evidence from the geological records, in When Did Plate Tectonics Begin on Planet Earth, Condie, K. and Pease, V., Eds., Spec. Pap.—Geol. Soc. Am., 2008, vol. 440, pp. 281–294.
Condie, K.C., High field strength element ratios in Archean basalts: a window to evolving sources of mantle plumes? Lithos, 2005, vol. 79, pp. 491–504.
Drummond, M.S. and Defant, M.J., A model for trondhjemite–tonalite-dacite genesis and crustal growth via slab melting: Archaean to modern comparison, J. Geophys. Res., 1990, vol. 95, pp. 21503–21521.
Egorova, Yu.S., Sanukitoids of Fenno-Karelian provinces of the Baltic Shield: geology, composition, sources, Extended Abstract of Cand. Sci. (Geol.-Mineral.) Dissertation, St. Peterburg, 2014.
Fitton, J.G., Sunders, A.D., Norry, M.J., et al., Thermal and chemical structure of the Iceland plume, Earth Planet. Sci. Lett., 1997, vol. 133, pp. 197–208.
Halla, J., Late Archean high-Mg granitoids (sanukitoids) in Southern Karelian Domain, eastern Finland: Pb and Nd isotopic constraints on crust–mantle interactions, Lithos, 2005, vol. 79, pp. 161–168.
Hamilton, W.B., Archean magmatism and deformation were not products of plate tectonics, Precambrian Res., 1998, vol. 91, pp. 143–179.
Huhma, H., Manttari, I., Peltonen, P., et al., The age of the Archaean greenstone belt of Finland, Geol. Surv. Finland. Spec. Pap., 2012a, vol. 12, pp. 73–174.
Huhma, H., Kontinen, A., Mikkola, P., et al., Nd isotopic evidence for Archaean crustal growth in Finland, Geol. Surv. Finland. Spec. Pap., 2012b, vol. 12, pp. 175–212.
Kozhevnikov, V.N., Arkheiskie zelenokamennye poyasa Karel’skogo kratona kak akkretsionnye orogeny (Archean Greenstone Belts of the Karelian Craton as Accretionary Orogens), Petrozavodsk: Izd. Karel. Nauchn. Tsentra Ross. Akad, Nauk, 2000 [in Russian].
Van Kranendonk, M.J., Tectonics of early Earth, in Earth’s Oldest Rocks, Van Kranendonk, M.J., Smithies, R.H., Bennett, V. C., Eds., Elsevier, 2007, pp. 1105–1116.
Kulikov, V.S., Simon, A.K., Kulikova, V.V., et al., Magmatic evolution of the Vodlozero block of the granitegreenstone terrane in the Archean, in Geologiya i geokhronologiya dokembriya Vostochno-Evropeiskoi platformy (Precambrian Geology and Geochronology of the East European Platform), Leningrad: Nauka, 1990, pp. 92–100.
Lobach-Zhuchenko, S.B., Arestova, N.A., Chekulaev, V.P., et al., Evolution of the South Vygozero Greenstone Belt, of Karelia, Petrology, 1999, vol. 7, no. 2, pp. 160–176.
Lobach-Zhuchenko, S.B., Chekulaev, V.P., Arestova, N.A., et al., Archean Terranes in Karelia: Geological and Isotopic-Geochemical Evidence, Geotectonics, 2000, vol. 34, pp. 452–466.
Martin, H., Adakitic magmas: modern analogues of Archaean granitoids, Lithos, 1999, vol. 46, pp. 411–429.
Myskova, T.A., Zhitnikova, I.A., Arestova, N.A., et al., New data about composition and age of rocks of the Shilossky Complex of Central Karelia, in Mat. Vseross. konf., posvyashchennoi 150-letiyu akademika F.Yu. Levinsona-Lessinga i 100-letiyu professora G.M. Saranchinoi (Proc. All-Russ. Conf. Devoted to 150-Annyversary of the Academician F.Yu. Levinson-Lessing and the 100th Anniversary of Prof. G.M. Saranchina “Modern Problems of Magmatism and Metamorphism”), St. Petersburg. State Univ., 2012, vol. 2, pp. 82–85.
Obshchaya stratigraficheskaya shkala nizhnego dokembriya Rossii. Ob”yasnitel’naya zapiska (General Stratigraphic Scale of the Lower Precambrian in Russia. Explanatory Note), Mitrofanov, F.P. and Negrutsa, V.Z., Eds., Apatity: Izd. Kolskogo Nauchn. Tsentra Ross. Akad, Nauk, 2002 [in Russian].
Polat, A., Kerrich, R., and Wyman, D.A., The late Archean Schreiber-Hemlo and White River-Dayohessarah greenstone belts, Superior Province: collages of oceanic plateaus, oceanic arcs, and subduction–accretion complexes, Tectonophysics, 1998, vol. 289, pp. 295–326.
Puchtel, I.S., Hofman, A.W., Mezger, A.W., et al., Oceanic plateau model for continental crustal growth in the Archaean: a case study from the Kostomuksha greenstone belt, NW Baltic Shield, Earth Planet. Sci. Lett., 1998, vol. 155, pp. 57–74.
Puchtel, I.S., Hofman, A.W., Amelin, Yu.V., et al., Combined mantle plume–island arc model for the formation of the 2.9 Ga Sumozero–Kenozero greenstone belt, SE Baltic Shield: isotope and trace element constraints, Geochim. Cosmochim. Acta, 1999, vol. 63, no. 21, pp. 3579–3595.
Rannii dokembrii Baltiiskogo shchita (Early Precambrian of the Baltic Shield), Glebovitskii, V.A., Ed., St. Petersburg: Nauka, 2005 [in Russian].
Said, N. and Kerrich, R., Geochemistry of coexisting depleted and enriched Paringa basalts in the 2.7Ga Kalgoorlie terrane, Yilgarn craton, Western Australia: for a heterogeneous mantle plume event, Precambrian Res., 2009, vol. 141, pp. 287–309.
Samsonov, A.V., Bogina, M.M., Bibikova, E.V., et al., The relationship between adakitic, calc-alkaline volcanic rocks and TTGs: implications for tectonic setting of the Karelian greenstone belts, Baltic Shield, Lithos, 2005, vol. 79, pp. 83–106.
Stern, R.J., Modern-style plate tectonics began in Neoproterozoic time: an alternative interpretation of earth’s tectonic history, in When did Plate Tectonic Begin on Planet Earth? Condie, K. and Pease, V., Eds., Spec. Pap.—Geol. Soc. Am., 2008, vol. 440, pp. 265–280.
Sun, S. and McDonough, W.F., Chemical and isotopic systematic of oceanic basalts: implications for mantle composition and processes, in Magmatism in the Ocean Basins, Saunders, A.D. and Norry, M.J., Eds., Geol. Soc. Spec. Publ., 1989, vol. 42, pp. 313–345.
Svetov, S.A., Magmaticheskie sistemy zony perekhoda okeankontinent v arkhee vostochnoi chasti Fennoskandinavskogo shchita (Magmatic Systems of the Ocean-Continent Transition Zone in the Archean in the Eastern Fennoscandian Shield), Petrozavodsk: Izd. Karel. Nauchn. Tsentra Ros. Akad. Nauk, 2005 [in Russian].
Svetov, S.A., Drevneishie adakity Fennoskandinavskogo shchita (Ancient Adakites of the Fennoscandian Shield), Petrozavodsk: Izd. Karel. Nauchn. Tsentra Ros. Akad. Nauk, 2009 [in Russian].
Vrevskii, A.B., Lobach-Zhuchenko, S.B., Chekulaev, V.P., et al., Geological, petrologic, isotopic, and geochemical constraints of geodynamic models simulating formation of the Archean tonalite-trondhjemite-granodiorite associations in ancient cratons, Geotectonics, 2010, vol. 44, no. 4, pp. 305–320.
Wyman, D.A., A 2.7 Ga depleted tholeiite suite: evidence of plume-arc interaction in the Abitibi greenstone belt, Canada, Precambrian Res., 1999, vol. 97, pp. 27–42.
Wyman, D.A., Kerrich, R., and Polat, A., Assembly of an Archean cratonic mantle lithosphere and crust: plume–arc interaction in the Abitibi–Wawa subduction–accretion complex, Precambrian Res., 2002, vol. 115, pp. 37–62.
Author information
Authors and Affiliations
Corresponding author
Additional information
Original Russian Text © V.P. Chekulaev, N.A. Arestova, Yu.S. Egorova, G.A. Kucherovskii, 2018, published in Stratigrafiya, Geologicheskaya Korrelyatsiya, 2018, Vol. 26, No. 3, pp. 3–23.
Rights and permissions
About this article
Cite this article
Chekulaev, V.P., Arestova, N.A., Egorova, Y.S. et al. Change of Conditions of the Formation of the Karelian Province of the Baltic Shield Continental Crust during Transition from Meso- to Neoarchean: Geochemical Study Results. Stratigr. Geol. Correl. 26, 243–260 (2018). https://doi.org/10.1134/S0869593818030048
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S0869593818030048