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Belarussian Basin

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Journal Article
Journal: PALAIOS
Published: 01 July 2017
PALAIOS (2017) 32 (7): 439–447.
...MAREK NARKIEWICZ; KATARZYNA NARKIEWICZ; EWA KRZEMIŃSKA; SEMEN A. KRUCHEK Abstract: Conodont apatite from a shallow-marine Middle Devonian transgressive unit has been investigated in five borehole sections representative of the epicontinental Belarussian Basin located in a near-equatorial setting...
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Journal Article
Journal: Geology
Published: 01 March 2009
Geology (2009) 37 (3): 271–274.
...E. Kiipli; T. Kiipli; T. Kallaste Abstract In the central part of the Mid-Ordovician–Early Silurian Baltic Basin, two different transport pathways of terrigenous material can be recognized. Kaolinite indicates the south-to-north sediment influx, and Cr the western and northern sources. A pathway...
FIGURES
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Paleogeographic location of the study area.  A ) Location of the Belarussia...
in > PALAIOS
Published: 01 July 2017
Fig . 1. Paleogeographic location of the study area. A ) Location of the Belarussian Basin (red dot) and other discussed areas on a map of Eifelian paleogeography (after Scotese 2002 ). Abbreviations: B–Czech Republic; G–Germany; MN–Montagne Noire, France. B) Middle Devonian paleogeography
Journal Article
Journal: Geology
Published: 22 March 2018
Geology (2018) 46 (5): 467–470.
... , https://doi.org/10.1017/S1089332600002552 . Narkiewicz , M. , Narkiewicz , K. , Krzeminska , E. , and Kruchek , S.A. , 2017 , Oxygen isotopic composition of conodont apatite in the equatorial epeiric Belarussian Basin (Eifelian)—Relationship to fluctuating seawater salinity...
FIGURES
Journal Article
Published: 05 June 2013
Geological Magazine (2014) 151 (2): 328–338.
... (N 79.2295, E 97.96872) a sequence of grey massive detrital limestones interbedded with claystones ( Fig. 3 ) is exposed along the unnamed creek in the basin of the Kan'on River ( Fig. 1 ). Limestones yield gastropods, crinoids and bryozoans. Locality B02_41 (N 79.21952, E...
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Journal Article
Published: 15 January 2010
Geological Magazine (2010) 147 (4): 527–550.
... Cross Mountains ( Fig. 1 ) (see e.g. Racki et al . 2002 ). Because detailed data concerning the previous stratigraphical and lithological studies of the deep-shelf (basinal) Kowala section have already been presented by Marynowski & Filipiak ( 2007 ), in the present paper we have described only...
Journal Article
Published: 01 May 2007
Geological Magazine (2007) 144 (3): 569–595.
... pericontinental basins along the southern margin of Laurussia ( Narkiewicz, 1988 ). In the late Frasnian to Famennian, due to expansion of the shelf-basinal system, most of the area was occupied by dark, clayey-calcareous deposits, which are commonly laminated, contain abundant early diagenetic pyrite, and lack...
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Journal Article
Journal: Palynology
Published: 01 June 2011
Palynology (2011) 35 (1): 4–45.
... (marls and argillaceous limestones) are found in southern Estonia and Latvia (Figure 1 ; Harris et al. 2004 ). The entire Baltoscandian region was surrounded in the north by the Fennoscandian Shield, in the south by the Belarussian Shield and in the east by the Moscow Basin (Figure 1...
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Series: Geological Society, London, Engineering Geology Special Publications
Published: 01 January 2010
DOI: 10.1144/EGSP23.11
EISBN: 9781862393851
... perpendicular to the ridge. Legend: 1, fault; 2, trench; 3, landslide main scarp; 4, debris-flow basin. Stereoplots show the orientation of main faults (mf) and tectonic conditions in the vicinity of the trenches. The Čertův Mlýn Mt. (1206 m) in the central part of the Moravskoslezské Beskydy Mts...
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Series: Mineralogical Society Series
Published: 01 January 2004
DOI: 10.1180/MSS.10.1
EISBN: 9780903056496
... during their emplacement was intraplate and extensional. Early Proterozoic carbonatites are connected, apparently, with the continental rifting of both the Karelian and Kola Cratons, which was taking place at ~2.2—2.0 Ga (Turchenko, 1992) . Numerous Palaeoproterozoic rift basins pass one...
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Series: Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.36
EISBN: 9781862394070
... represent a c . 1.84 Ga rim of crustal growth in the Polish–Lithuanian terrane, similar to the 1.83–1.82 Ga Oskarshamn-Jönköping Belt in southeastern Sweden ( Mansfeld 1996 ; Mansfeld et al . 2005 ). The former presence of an oceanic basin between the Polish–Lithuanian and Lithuanian-Belarus terranes...
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