Abstract
The dike-vein complex of the Moncha Tundra Massif comprises dolerites, gabbro-pegmatites, and aplites. The dolerite dikes are classified into three groups: high-Ti ferrodolerites, ferrodolerites, low-Ti and low-Fe gabbro-dolerites. The U-Pb age of the ferrodolerites is 2505 ± 8 Ma, and the amphibole-plagioclase metagabbroids hosting a ferrodolerite dike are dated at 2516 ± 12 Ma. Data on the U-Pb isotopic system of zircon from the gabbro-pegmatites and titanite from the aplites indicate that the late magmatic evolution of the Moncha Tundra Massif proceeded at 2445 ± 1.7 Ma, and the youngest magmatic events in the massif related to the Svecofennian orogeny occurred at 1900 ± 9 Ma. The data obtained on the Sm-Nd and Rb-Sr isotopic systems and the distribution of trace elements and REE in rocks of the dike-vein complex of the massifs provide insight into the composition of the sources from which the parental magmas were derived. The high-Ti ferrodolerites were melted out of a deep-sitting plume source that contained an asthenospheric component. The ferrodolerites were derived from a mantle MORB-type source that contained a crustal component. The parental melts of the gabbro-dolerites were melted out of the lithospheric mantle depleted in incompatible elements after Archean crust-forming processes above an ascending mantle plume, with the participation of a crustal component. The gabbro-dolerites and the rocks of the layered complex of the Moncha Tundra Massif exhibit similar geochemical characteristics, which suggest that their parental melts could be derived from similar sources but with more clearly pronounced crustal contamination of the parental melts of the rocks of the massif itself. The geochemical traits of the gabbro-pegmatites are thought to be explained not only by the enrichment of the residual magmas in trace elements and a contribution of a crustal component but also by the uneven effect of sublithospheric mantle sources. The aplites were derived from a sialic crustal source.
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References
F. P. Mitrofanov, “Prospecting indicators of new economic-grade Rh-Pt-Pd, Co-Cu-Ni, and Cr deposits at the Kola Peninsula,” Otechestvennaya Geol., No. 4, 3–9 (2006).
Layered Intrusions of the Monchegorsk Ore District: Petrology, Mineralization, and Deep Structure, Ed. by F.P. Mitrofanov and V.F. Smol’kin (Izd. KNTs RAN, Apatity, 2004), Vol. 1 [in Russian].
A. A. Arzamastsev, Zh. A. Fedotov, and L. V. Arzamastseva, Dike Magmatism of the Northeastern Baltic Shield (Nauka, St. Petersburg, 2009) [in Russian].
E. K. Kozlov, B. A. Yudin, and V. S. Dokuchaeva, Mafic and Ultranafic Complexes of the Moncha-Volch’iLosevy Tundras (Nauka, Leningrad, 1967) [in Russian].
T. B. Bayanova, L. I. Nerovich, F. P. Mitrofanov, P. A. Serov, and V. A. Zhavkov, “The Monchetundra basic massif of the Kola Region: new geological and isotope geochronological data,” Dokl. Earth Sci. 431(1), 288–293 (2010).
T. Bayanova, J. Ludden, and F. Mitrofanov, “Timing and duration of Paleoproterozoic events producing orebearing layered intrusions of the Baltic Shield: metallogenic, petrological and geodynamic implications,” Geol. Soc. London Sp. Publ. 323, 165–198 (2009).
L. I. Nerovich, T. B. Bayanova, E. E. Savchenko, P. A. Serov, and N. A. Ekimova, “New data on the geology, petrography, isotope geochemistry and PGE mineralization of the Moncha Tundra Massif,” Vestnik Murm. Gos. Tekhn. Univ. 12(3), 461–477 (2009).
V. I. Pozhilenko, B. V. Gavrilenko, D. V. Zhirov, and S. V. Zhabin, Geology of the Ore Districts of the Murmansk Region (Izd. KNTs RAN, Apatity, 2002) [in Russian].
T. E. Krogh, “A low-contamination method for hydrothermal dissolution of zircon and extraction of U and Pb for isotopic age determinations,” Geochim. Cosmohim. Acta 37, 485–494 (1973).
T. B. Bayanova, Age of the Reference Geological Complexes of the Kola Region and Duration of Magmatic Processes (Nauka, St. Petersburg, 2004) [in Russian].
T. B. Bayanova, F. Corfu, V. Todt, U. Poller, N. V. Levkovich, E. A. Apanasevich, and V. A. Zhavkov, “Heterogeneity of 91500 and TEMORA-1 standards for single zircon dating,” in Processsing of 18th Vinogradov Symposium on Isotope Geochemistry, Moscow, Russia, 2007 (GEOKhI, Moscow, 2007), pp. 42–43 [in Russian].
J. S. Stasey and J. D. Kramers, “Approximation of terrestrial lead isotope evolution by a two-stage model,” Earth Planet. Sci. Lett. 26, 207–221 (1975).
K. R. Ludwig, “ISOPLOT-a plotting and regression program for radiogenic-isotope data, Version 2.56,” US Geol. Surv. Open-file Rept. 91-445 (1991).
K. R. Ludwig, “ISOPLOT/Ex-a geochronological toolkit for Microsoft Excel, Version 2.05,” Berkeley Geochronol. Center Sp. Publ., No. 1a, (1999).
R. H. Steiger and E. Jager, “Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology,” Earth Planet. Sci. Lett. 36(3), 359–362 (1977).
A. Z. Zhuravlev, D. Z. Zhuravlev, Yu. A. Kostitsyn, and I. V. Chernyshov, “Determination of Sm/Nd ratio for geochronological aims,” Geokhimiya, No. 8, 1115–1129 (1987).
D. J. De Paolo, “Neodymium isotopes in the Colorado Front Range and crust-mantle evolution in the Proterozoic,” Nature 291, 193–196 (1981).
S. V. Panteeva, D. P. Gladkochoub, T. V. Donskaya, V. V. Markova, G. P. Sandimirova, “Determination of 24 trace elements in felsic rocks by inductively coupled plasma mass spectrometry after lithium metaborate fusion,” Spectrochim. Acta, Part B: Atom. Spectroscop. 58(2), 341–350 (2003).
Zh. A. Fedotov, P. A. Serov, and D. V. Elizarov, “Tholeiites from the depleted subcontinental mantle in the root zone of the Monchegorskii Pluton, Baltic Shield,” Dokl. Earth Sci. 429A(9), 1462–1466 (2009).
K. Putirka, “Clinopyroxene+liquid equilibria to 100 kbar and 2450 K,” Contrib. Mineral. Petrol. 135, 151–163 (1999).
I. D. Ryabchikov, “Mantle magmas as a sensor of the composition of deep geospheres,” Geol. Rudn. Mestorozhd. 47(6), 455–468 (2005).
A. W. Hofmann, “Mantle geochemistry: the message from oceanic volcanism,” Nature 385, 219–229 (1997).
J. A. Pearce, “Role of the sub-continental lithosphere in magma genesis at active continental margins,” in Continental Basalts and Mantle Xenoliths: Papers Prepared for a UK Volcanic Studies Group Meeting at the University of Leicester (Shiva, Nantwich, 230–249).
K. Y. Tomlinson and K. C. Condie, “Archean mantle plumes: evidence from greenstone belt geochemistry,” in Mantle Plumes: Their Identification Through Time, Geol. Soc. Am., Spec. Pap. 352, 341–358 (2001).
K. C. Condie, “High field strength element ratios in Archean basalts: a window to evolving sources of mantle plumes?,” Lithos 79, 491–504 (2005).
O. M. Turkina, Lectures on the Geochemistry of the Mantle and Continental Crust. A Textbook (Izd. Novosib. Gos. Univ., Novosibirsk, 2007) [in Russian].
W. V. Boynton, “Cosmochemistry of the rare earth elements: meteorite studies,” in Rare Earth Element Geochemistry, Ed. by P. Henderson (Elsevier, Amsterdam, 1984), pp. 63–114.
S. S. Sun and W. F. McDonough, “Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes,” in Magmatism in the Oceanic Basins, Ed. by A.D. Saunders and M.J. Norry, Geol. Soc. London, Spec. Publ, No. 42, 313–345 (1989).
V. F. Smol’kin, Early Precambrian Komatiitic and Picritic Magmatism of the Baltic Shield (Nauka, St. Petersburg, 1992) [in Russian].
Magmatism, Sedimentogenesis, and Geodynamics of the Pechenga Paleorift Structure, Ed. by F. P. Mitrofanov and V. F. Smol’kin (Izd. KNTs RAN, Apatity, 1995) [in Russian].
E. V. Sharkov, V. F. Smol’kin, V. B. Belyatskii, A. V. Chistyakov, and Zh. A. Fedotov, “Age of the Moncha Tundra Fault, Kola Peninsula: evidence from the Sm-Nd and Rb-Sr isotopic systematics of metamorphic assemblages,” Geochem. Int. 44(4), 317–326 (2006).
D. J. Cherniak, “Lead diffusion in titanite and preliminary results on the effects of radiation damage on Pb transport,” Chem. Geol. 110, 177–194 (1993).
B. R. Frost, K. R. Chamberlain, and J. C. Schumacher, “Sphene (titanite): phase relations and role as a geochronometer,” Chem. Geol. 172, 131–148 (2000).
V. A. Melezhik and B. A. Sturt, “General geology and evolutionary history of the Early Proterozoic Polmak-Pasvik-Pechenga-Imandra/Varzuga-Ust-Ponoy greenstone belt in the northeastern Baltic Shield,” Earth-Sci. Rev. 36, 205–241 (1994).
C. Dupuy, A. Michard, J. Dostal, D. Dautel, and W. R. A. Baregar, “Isotope and trace-element geochemistry of Proterozoic Natkusiak flood basalts from the Northwestern Canadian Shield,” Chem. Geol. 120, 15–25 (1995).
G. L. Farmer, “Continental Basaltic Rocks,” Treatise Geochem. 3, 85–121 (2003).
J. H. Puffer, “Late Neoproterozoic Eastern Laurentian Superplume: location, size, chemical composition, and environmental impact,” Amer. J. Science 302, 1–27 (2002).
A. A. Nosova, O. F. Kuz’menkova, N. V. Veretennikov, L. G. Petrova, and L. K. Levskii, “Neoproterozoic Volhynia-Brest magmatic province in the western East European Craton: within-plate magmatism in an ancient suture zone,” Petrology 16(2), 115–147 (2008).
A. A. Shchipanskii, Subduction and Mantle-Plume Processes in the Geodynamics of the Formation of the Archean Greenstone Belts (Izd. LKI, Moscow, 2008) [in Russian].
F. P. Lesnov, Rare-Earth Elements in the Ultramafic and Mafic Rocks and Their Minerals (Geo, Novosibirsk, 2007), vol. 1 [in Russian].
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Original Russian Text © L.I. Nerovich, T.B. Bayanova, P.A. Serov, D.V. Elizarov, 2014, published in Geokhimiya, 2014, No. 7, pp. 605–624.
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Nerovich, L.I., Bayanova, T.B., Serov, P.A. et al. Magmatic sources of dikes and veins in the Moncha Tundra Massif, Baltic Shield: Isotopic-geochronologic and geochemical evidence. Geochem. Int. 52, 548–566 (2014). https://doi.org/10.1134/S0016702914070052
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DOI: https://doi.org/10.1134/S0016702914070052