Коллектив авторов - Строение и история развития литосферы

Kuznetsov N.B., Soboleva A.A., Udoratina O.V. et al. Pre-Ordovician tectonic evolution and volcano – plutonic associations of the Timanides and northern Pre-Uralides, northeast part of the East European Craton // Gondwana Research. 2007. V.12. P. 305–323. doi:10.1016/j.gr.2006.10.021

Larionov A.N., Andreichev V.L., Gee D. The Vendian alkaline igneous suites of northern Timan: ion microprobe U-Pb zircon ages of gabbros and syenite // The Neoproterozoic Timanide Orogen of Eastern Baltica / Gee D.G., Peas, V. (eds.) Geological Soc., London. 2004. Mem. 30. P. 69–74.

Larionov A.N., Teben’kov A.M. New SHRIMP-II U-Pb zircon age data from granitic boulders in Vendian tillited of southern coast of Isfjorden, West Spitsbergen. Arctic Geology, Hydrocarbon Resources and Environmental Chqllenges // NGF. 2004. N2. P. 88–89.

Leech M.L., Willingshofer E.G. Thermal modeling of the UHP Maksyutov Complex in the south Urals // Earth and Planetary Science Letters. 2004. Vol. P. 85–99

Li Z.X., Bogdanova S.V., Collins A.S. et al. Assembly, configuration, and break-up history of Rodinia: A synthesis // Precambrian Res. 2008. Vol. 160. P. 179–210

Linnemann U., Romer R.L. The Cadomian orogeny in Saxo-Thuringia, Germany: Geochemical and Nd-Sr-Pb isotopic characterization of marginal basins with constraints to geotectonic setting and provenance // Tectonophysics. 2002. V. 352. P. 33–64.

Linnemann U., McNaughton N. J., Romer R. L. et al. West African provenance for Saxo-Thuringia (Bohemian Massif): Did Armorica ever leave pre-Pangean Gondwana? – U/Pb-SHRIMP zircon evidence and the Nd-isotopic record // Int. J. Earth Sci. (Geol. Rundsch.), 2004. 93, p. 683–705.

Linnemann U., Gerdes A., Drost K., Buschmann B. The continuum between Cadomian orogenesis and opening of the Rheic Ocean: Constraints from LA-ICP-MS U-Pb zircon dating and analysis of plate-tectonic setting (Saxo-Thuringian zone, northeastern Bohemian Massif, Germany). The evolution of the Rheic Ocean: From Avalonian-Cadomian active margin to Alleghenian-Variscan collision // Geol. Soc. Am. Sp. Paper. 2007. 423: p. 61–96.

Llanos I., Tait M.P., Popov J.A., Ablama-sova A. Paleomagnetic data from Ediacaran (Vendian) sediments of the Arkhangelsk region, NW Russia: an alternative apparent polar wander path of Baltica for the Late Proterozoic – Early Palaeozoic // Earth and Planetary Science Letters. 2005. Vol.240. P. 732–747.

Lorenz H. Eurasian Arctic Tectonics: Geology of Severnaya Zemlya (North Kara Terrane) and Relationships to the Timanide Margin of Baltica. Acta Universitatis Upsaliensis. Upsala. 2005. 93p.

Lorenz H., Gee D.G., Simonetti A. Detrital zircon ages and provenance of the Late Neoproterozoic and Palaeozoic successions on Severnaya Zemlya, Kara Shelf: a tie to Baltica // Norwegian Journal of Geology 2008. v. 88. Р. 235–258.

Majka J., Czerny J., Manecki M., Mazur S. New evidence for a late Neoproterozoic (ca. 650 Ma) metamorphic event in the Caledonian basement of Wedel Jarlsberg Land, West Spitsbergen. European Geosciences Union. 2007. Geophysical Research Abstracts. 2007a. V. 9. 00923. SRef-ID: 1607–7962/gra/EGU2007-A-00923

Majka J., Gee D.G., Larionov A. et al. Neoproterozoic Zircon Age From Anathectic Pegmatite, Isborhamna Group (Wedel Jarlsberg Land, Svalbard). NGF № 2, 2007b. Abstract and Proceedings of the Geological Society of Norway. Abstract No ISP-041. P. 266.

Majka J., Mazur S., Manecki M. et al. Late Neoproterozoic amphibolite-facies metamorphism of a pre-Caledonian basement block in southwest Wedel Jarlsberg Land, Spitsbergen: new evidence from U – Th – Pb dating of monazite // Geol. Mag. 2008, P. 1–9. Cambridge University Press. doi:10.1017/S001675680800530X.

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Maslov A.V. Riphean and Vendian sedimentary sequences of the Timanides and Uralides, the eastern periphery of the East European Craton. In: The Neoproterozoic Timanide Orogen of Eastern Baltica. Gee D. G. and Pease V. (Eds.). Geological Soc., London. Memoirs. 30. 2004. p. 19–35.

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Miller E.L., Gehrels G.E., Pease V., Sokolov S. Paleozoic and Mesozoic stratigraphy and U-Pb detrital zircon geochronology of Wrangel Island, Russia: Constraints on paleogeography and paleocontinental reconstructions of the Arctic // AAPG Bulletin 2009. (in press)

Moczydlowska M., Stockfors M., Popov L. Late Cambrian relative age constraints by acritarchs on the post-Timanian deposition on Kolguev Island, Arctic Russia. London. Geological Society. 2004. Memoirs V. 30. p. 159–168. doi:10.1144/GSL.MEM.2004.030.01.14 2004

Moore T. Potter, C.J.; O’Sullivan, Aleinikoff J.N. Detrital zircons U-Pb ages from Pre-Missippian rocks and Unconformaly overlying strata of the Mississipian to Triassic Ellesmerian and Jurassic and Lower Cretaceous Beaufortian sequences, Western Brooks Range and North slope, Alaska // NGF2007. ICAM-V. p. 124

Murphy J.B., Strachan R.A., Nance R.D. et al. Proto-Avalonia: A 1.2–1.0 Ga tectonothermal event and constraints for the evolution of Rodinia // Geology. 2000. V. 28. P. 1071–1074.

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Nicoll G.R., Tait J.A., Zimmerman U. Provenance analysis and tectonic setting of Neoproterozoic sediments on the Varanger Peninsula, Northern Norway. In: Rodinia: Supercontinents, Superplumes and Scotland, Fermor meeting, Programme and abstracts. Edinburg, Scotland, 2009, P. 68.

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Pease V. East European craton margin source for the allochthonous Northern Terrane of Taimyr, Arctic Siberia. EOS Transactions, American Geophysical Union. 2001a. 82, 47, F1181.

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Pease V., Scott R.A. Crustal affinities in the Arctic Uralides, northern Russia: significance of detrital zircon ages from Neoproterozoic and Palaeozoic sediments in Novaya Zemlya and Taimyr // Journal of the Geological Society 2009; v. 166; p. 517–527.

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Abstract

The newest data (been obtained during the recent years, partially in the frames of IPY programs) over the Western Arctic regions and (to a lesser degree) over some other areas of Arctic are presented. They concern the internal structure Neoproterozoic complexes of some areas of the Western Arctic regions and obtaining of geochemical, isotopic-geochemical and isotopic-geochronological characteristics of detrital zircons from silicaclactic rocks from few Neoproterozoic units of the Timan and Polar Urals. Summary of the presented data and the newest various data (geochronological, petrological, biogeographical, etc.) from other high-latitude areas of Arctica allowed to consider Neoproterozoic – Early Paleozoic tectonic history of Arctica, particularly, a problem of existence of an ancient (Precambrian) continent Arctida/Hyperborea whose fragments are now distributed over the Arctic sector.