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Belomorian Belt

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Journal Article
Published: 01 March 2012
Russ. Geol. Geophys. (2012) 53 (3): 262–280.
...A.A. Shchipansky; L.I. Khodorevskaya; A.I. Slabunov Abstract We present results of geochemical studies and isotope dating of eclogites and associated rocks from the Kuru-Vaara quarry, Belomorian Belt, Northeastern Baltic Shield. The southern and northern eclogites are similar in geochemical...
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Journal Article
Published: 01 January 2012
Russ. Geol. Geophys. (2012) 53 (1): 1–21.
...A.A. Shchipansky; L.I. Khodorevskaya; A.N. Konilov; A.I. Slabunov Abstract The paper focuses on the metamorphic geology of the oldest crustal eclogites discovered in the Late Archean tonalite-trondhjemite-granodiorite (TTG) complex of the Belomorian Mobile Belt on the Kola Peninsula. Eclogite...
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Journal Article
Published: 01 May 2015
Russ. Geol. Geophys. (2015) 56 (5): 709–728.
...V.M. Kozlovskii; L.Ya. Aranovich; N.I. Frishman Abstract Plagioclase-bearing garnet–omphacite (Grt–Omp) eclogites and garnet–augite eclogite-like (Grt–Aug) schists from the amphibolite and gneiss beds of the Belomorian Mobile Belt have been studied. They are spread over a large area. In most...
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Geology of Karelia and the <b>Belomorian</b> <b>Belt</b> with study locations. (A) Tecton...
Published: 01 April 2014
Figure 1. Geology of Karelia and the Belomorian Belt with study locations. (A) Tectonic and igneous architecture of Kola and Karelia separated by the Belomorian Belt; note the NW-SE–trending rifts of 2.4–2.5 Ga. The degree of metamorphism increases from the Vetreny-Shambozero-Kuolasjarvi Belts
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Geology of Karelia and the <b>Belomorian</b> <b>Belt</b> with study locations. (A) Tecton...
Published: 01 April 2014
Figure 1. Geology of Karelia and the Belomorian Belt with study locations. (A) Tectonic and igneous architecture of Kola and Karelia separated by the Belomorian Belt; note the NW-SE–trending rifts of 2.4–2.5 Ga. The degree of metamorphism increases from the Vetreny-Shambozero-Kuolasjarvi Belts
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Schematic position of the <b>Belomorian</b> <b>Belt</b> in the structure of the eastern B...
Published: 01 January 2012
Fig. 1. Schematic position of the Belomorian Belt in the structure of the eastern Baltic Shield. The study area is shown by a rectangle (see Fig. 2 ). Asterisk shows the position of the first world finding of the Archean Gridino crustal eclogites (Gr), and white asterisk, the position
Image
Simplified geologic map of <b>Belomorian</b> <b>belt</b> with structural elements ( Balag...
Published: 01 July 2010
Figure 1. Simplified geologic map of Belomorian belt with structural elements ( Balagansky et al., 1986 ; Bibikova et al., 2004 ), showing locations of Paleoproterozoic Chupa allochthonous nappe with Khitostrov corundum plagiogneisses (1x), low δ 18 O plagiogneiss of Mount Dyadina (2x
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Paleogeographic setting of <b>Belomorian</b> <b>belt</b>. Superior craton (gridded, unsha...
Published: 01 July 2010
Figure 4. Paleogeographic setting of Belomorian belt. Superior craton (gridded, unshaded) and Kola and Karelia (gridded, shaded) are reconstructed through time, to paleolatitudes (Mercator projection) and orientations according to named paleomagnetic poles (ages in Ma) ( Mertanen et al., 2006
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Geological map of the <b>Belomorian</b> <b>Belt</b> in the White Sea area (after Glebovit...
Published: 01 May 2004
F igure 1. Geological map of the Belomorian Belt in the White Sea area (after Glebovitsky et al. 1996). 1 = Keretz nappe, 2 = Chetolambin nappe, 3 = mafic rocks of the Chetolambin nappe, 4 = Archaean supracrustal rocks of the Pongoma and Gridino area, 5 = Chupa nappe, 6 = Orijärvi nappe, 7
Journal Article
Journal: Geosphere
Published: 01 April 2014
Geosphere (2014) 10 (2): 308–339.
...Figure 1. Geology of Karelia and the Belomorian Belt with study locations. (A) Tectonic and igneous architecture of Kola and Karelia separated by the Belomorian Belt; note the NW-SE–trending rifts of 2.4–2.5 Ga. The degree of metamorphism increases from the Vetreny-Shambozero-Kuolasjarvi Belts...
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Schematic geologic structure of the southeastern part of the <b>Belomorian</b>–Lap...
Published: 01 May 2015
Fig. 1. Schematic geologic structure of the southeastern part of the Belomorian–Lapland belt, after Kolodyazhnyi (2006) , with marked high-pressure metamorphism objects (our data). 1 – 7 , Neoarchean deposits of the Belomorian Belt; 8 – 15 , Paleoproterozoic deposits of the Kolvitsa–Umba
Journal Article
Published: 01 May 2004
American Mineralogist (2004) 89 (5-6): 819–831.
...F igure 1. Geological map of the Belomorian Belt in the White Sea area (after Glebovitsky et al. 1996). 1 = Keretz nappe, 2 = Chetolambin nappe, 3 = mafic rocks of the Chetolambin nappe, 4 = Archaean supracrustal rocks of the Pongoma and Gridino area, 5 = Chupa nappe, 6 = Orijärvi nappe, 7...
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Schematic geological map of northwestern Fennoscandian shield, showing samp...
Published: 01 August 2010
Figure 1. Schematic geological map of northwestern Fennoscandian shield, showing sample locations. (For detailed three-dimensional image of Belomorian belt, see Mints et al. [2009] .)
Journal Article
Journal: Geology
Published: 01 July 2010
Geology (2010) 38 (7): 631–634.
...Figure 1. Simplified geologic map of Belomorian belt with structural elements ( Balagansky et al., 1986 ; Bibikova et al., 2004 ), showing locations of Paleoproterozoic Chupa allochthonous nappe with Khitostrov corundum plagiogneisses (1x), low δ 18 O plagiogneiss of Mount Dyadina (2x...
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Journal Article
Journal: Geology
Published: 01 July 2017
Geology (2017) 45 (7): 667–670.
... on the Baltic Shield as the result of global mantle plume activity in early Paleoproterozoic (Sumian) time ( Amelin et al., 1995 ; Kulikov et al., 2010 ). The Belomorian belt, located in Karelia, Russia, between the Karelian and Kola cratons ( Fig. 1 ), was a zone of extensive rifting from 2.44 to 2.39 Ga...
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Indicator geochemical diagrams depicting the genetic features of the protol...
Published: 01 March 2012
Fig. 9. Indicator geochemical diagrams depicting the genetic features of the protoliths of Archean eclogites at the Kola segment of the Belomorian Belt. a , Th-Yb proxy (Th-Nb crustal input proxy) diagram ( Pearce, 2008 ). ACC and CC, Archean continental crust and continental crust, respectively
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Zircon ages and δ 18 O values determined by ion microprobe in sample K5 dem...
Published: 01 July 2010
. A: Age histogram; gray bands denote published ion microprobe zircon ages from other rocks across Belomorian belt ( Bibikova et al., 2004 ; Serebryakov et al., 2007 ) showing similar age patterns: 1—rims of zircons in similar pegmatites, 2—zircons from regional gabbro, 3—predominant detrital zircons
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Schematic probable occurrence of eclogites in the structure of the northeas...
Published: 01 January 2012
Fig. 2. Schematic probable occurrence of eclogites in the structure of the northeastern Belomorian Belt, with localities where isotope-geochronological data were obtained. Constructed using data of scale 1 : 200,000 geological surveys ( Konilov et al., 2011 ; Mints et al., 2010 ; Pozhilenko et
Journal Article
Published: 01 May 2021
Russ. Geol. Geophys. (2021) 62 (5): 525–546.
...A.I. Slabunov; V.V. Balagansky; A.A. Shchipansky Abstract —The Belomorian Province (BP) of the Fennoscandian Shield is a high-grade belt composed of Meso- to Neoarchean tonalite– trondhjemite–granodiorite (TTG) gneisses with subordinate supracrustal complexes. The Belomorian crust is underlined...
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Journal Article
Journal: Geology
Published: 01 August 2010
Geology (2010) 38 (8): 739–742.
...Figure 1. Schematic geological map of northwestern Fennoscandian shield, showing sample locations. (For detailed three-dimensional image of Belomorian belt, see Mints et al. [2009] .) ...
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