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Vrevskii, A. B. (2019) Non-Subduction Petrological Mechanisms for the Growth of the Neoarcheam Continental Crust of the Kola–Norwegian Terrane, Fennoscandian Shield: Geological and Isotope-Geochemical Evidence. Petrology, 27 (2) 146-170 doi:10.1134/s0869591119020073

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Reference TypeJournal (article/letter/editorial)
TitleNon-Subduction Petrological Mechanisms for the Growth of the Neoarcheam Continental Crust of the Kola–Norwegian Terrane, Fennoscandian Shield: Geological and Isotope-Geochemical Evidence
JournalPetrology
AuthorsVrevskii, A. B.Author
Year2019 (March)Volume27
Issue2
PublisherPleiades Publishing Ltd
DOIdoi:10.1134/s0869591119020073Search in ResearchGate
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Mindat Ref. ID506928Long-form Identifiermindat:1:5:506928:0
GUID0
Full ReferenceVrevskii, A. B. (2019) Non-Subduction Petrological Mechanisms for the Growth of the Neoarcheam Continental Crust of the Kola–Norwegian Terrane, Fennoscandian Shield: Geological and Isotope-Geochemical Evidence. Petrology, 27 (2) 146-170 doi:10.1134/s0869591119020073
Plain TextVrevskii, A. B. (2019) Non-Subduction Petrological Mechanisms for the Growth of the Neoarcheam Continental Crust of the Kola–Norwegian Terrane, Fennoscandian Shield: Geological and Isotope-Geochemical Evidence. Petrology, 27 (2) 146-170 doi:10.1134/s0869591119020073
In(2019, March) Petrology Vol. 27 (2) Pleiades Publishing Ltd

See Also

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Vrevskii, A. B. (2018) Specifics of Neoarchean Plume–Lithospheric Processes in the Kola–Norwegian Province of the Fennoscandian Shield: I. Composition and Age of the Komatiite–Tholeiite Association. Petrology, 26 (2) 121-144 doi:10.1134/s0869591118020066
Vrevskii, A. B. (2018) Specifics of the Neoarchean Plume–Lithospheric Processes in the Kola–Norwegian Province of the Fennoscandian Shield: II. Petrology and Geodynamic Nature of Komatiite–Tholeiite Association. Petrology, 26 (3) 246-254 doi:10.1134/s0869591118030074
Vrevskii, A. B. (2009) Geochemical and isotopic signatures of nonsubduction mechanisms of formation of the Neoarchean continental lithosphere of the Fennoscandian shield. Doklady Earth Sciences, 429 (2) 1575-1579 doi:10.1134/s1028334x09090347
Vrevskii, A. B. (2016) Age and sources of the anorthosites of the Neoarchean Kolmozero-Voron’ya greenstone belt (Fennoscandian Shield) Petrology, 24 (6) 527-542 doi:10.1134/s0869591116060060
Vrevsky, A. B., Kuznetsov, A. B., Lvov, P. A. (2023) Age and Stratigraphic Position of a Supracrustal Complex (Kaskama Block, Inari Terrane, Northeastern Kola–Norwegian Region of the Fennoscandian Shield) Doklady Earth Sciences, 511 (2) Pleiades Publishing Ltd. 645-651 doi:10.1134/s1028334x23600950
Vrevskii, A.B. (2021) The Ludicovian of the Raahe–Ladoga Zone of the Fennoscandian Shield (Isotope-Geochemical Composition and Geodynamic Nature) Russian Geology and Geophysics, 62 (10) 1089-1106 doi:10.2113/rgg20204173
Vrevskii, A. B., Turchenko, S. I. (2021) Age, Isotopic Features, and Formation Type of Rocks and Ores of the Allarechka Cu–Ni Sulfide Deposit, Fennoscandian Shield. Petrology, 29 (4) 351-370 doi:10.1134/s0869591121040081
Vrevsky, A. B., Kuznetsov, A. B., Lvov, P. A. (2024) New Data on the Regional Stratigraphic Scale of the Paleoproterozoic of the Fennoscandian Shield (Isotope Geochemistry and Age of Supracrustal Rock Complexes of the Inari Terrane, Kola Peninsula). Doklady Earth Sciences, 519 (1). doi:10.1134/s1028334x24602773
(1993) The growth of continental crust during the Late Proterozoic: geochemical evidence from the Arabian Shield. Special Publication, 76. Geological Society of London. 363-371 doi:10.1144/gsl.sp.1993.076.01.18
Gusev, N. I., Sergeeva, L. Yu., Skublov, S. G. (2021) Evidence of Subduction of the Paleoproterozoic Oceanic Crust in the Khapchan Belt of the Anabar Shield, Siberian Craton. Petrology, 29 (2) 95-113 doi:10.1134/s0869591121020041
Kovach, V. P., Yarmolyuk, V. V., Kovalenko, V. I., Kozlovskyi, A. M., Kotov, A. B., Terent’eva, L. B. (2011) Composition, sources, and mechanisms of formation of the continental crust of the Lake zone of the Central Asian Caledonides. II. Geochemical and Nd isotope data. Petrology, 19 (4) 399-425 doi:10.1134/s0869591111030064
 
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