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Brunia

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Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.9
EISBN: 9781862396814
... of the Teplá–Barrandian upper crust, exhumation of the high-grade (Moldanubian) core of the orogen at c. 346–337 Ma and by dextral strike-slip along orogen-perpendicular NW–SE shear zones; (3) following closure of a Rhenohercynian Ocean basin, the Brunia microplate was underthrust beneath the eastern flank...
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Journal Article
Published: 15 January 2010
Geological Magazine (2010) 147 (4): 508-526.
... in the adjacent Sudetic part of the Bohemian Massif and are considered characteristic of peri-Gondwanan crust. Our data prove the dissimilarity between the Brunia plate and the westerly terranes of the Variscan belt. The occurrence of granitic gneisses with late Neoproterozoic protolith ages and widespread...
Journal Article
Published: 01 March 2000
Journal of the Geological Society (2000) 157 (2): 401-416.
... of a continental accretionary wedge; (3) eduction of the wedge and Late Carboniferous transpression. Devonian rifting of the Brunia microcontinent resulted in the formation of two crustal‐scale boudins associated with the development of two syn‐rift Devonian basins. This extensional template strongly influenced...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.09
EISBN: 9781862394278
.... Samples from the Silesian Domain (Desná Dome, Staré Město Belt, Velké Vrbno Unit) of the Brunia Microcontinent, in thrust contact with the Lugian Domain, yielded Nd crustal residence ages of 1.1–1.3 Ga, which coincide with the oldest ages of xenocrystic zircons. Brunia is interpreted as a predominantly...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.12
EISBN: 9781862394278
... facies conditions. There are few precise ages for rocks in the area under discussion. Van Breeman et al. (1982) reported multigrain U–Pb zircon data for the Keprník gneiss and the Brno pluton, both part of the Brunia domain, and a Rb–Sr isochron age for the Snierzník gneiss of the Lugian domain...
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Image
Schematic map of the Bohemian Massif and the studied Variscan granitoids (m...
Published: 01 February 2017
; ST, Saxothuringian Unit; M, Moldanubian Unit; B, Brunia Continent; L, Lugian domain.
Image
Inferred heterogeneous channel flow within the Moldanubian region, Bohemian...
in > Elements
Published: 01 August 2011
) and orogenic middle crust (green and orange), flowed over strong continental crust (Brunia, pink) during late Paleozoic collision. CMP = Central Moldanubian Pluton; OMC = orogenic middle crust; OLC = orogenic lower crust
Image
Peri-Gondwanan terranes of southern and central Europe (modified from  Linn...
Published: 01 December 2016
– Bristol Channel-Bray Fault; BM – Bohemian Massif; Br – Brunia; CS – Central Sudetes; EB – Elbe Fault; FMC – French Massif Central; Ga – Ganderia; ISF – Intra-Sudetic Fault; IS – Iapetus suture; MC – Midland craton; MZ – Moldanubian zone; OF – Odra Fault; RM – Rhenish Massif; RS – Rheic suture; ST – Saxo
Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.14
EISBN: 9781862396814
... b ). The Neoproterozoic Brunia continent can be subdivided into: The ‘Moravo-Silesian Zone’ of Suess (1912 , 1926 ), which corresponds to the tectonic transition zone between the Moldanubian units, was thrust over the Brunia continent. The boundary between the Moldanubian and Moravo-Silesian...
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Journal Article
Journal: Geology
Published: 01 April 2014
Geology (2014) 42 (4): 275-278.
...) a Late Devonian–early Carboniferous magmatic arc (Central Bohemian Plutonic Complex); (5) a deep crustal root (Moldanubian domain); and (6) a buttress continent (Brunia). Recent advances (summarized in Lexa et al., 2011 ) have enabled the definition of plate affinities for individual crustal units...
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Journal Article
Published: 01 January 2014
Journal of the Geological Society (2014) 171 (1): 83-95.
... 2005 ; Racek et al . 2006 ; Franěk et al . 2006 , 2011 ; Tajčmanová et al . 2006 , 2010 ). In the east, the Moldanubian rocks are thrust over the basement of the Neoproterozoic Brunovistulian block (Brunia). Their mutual collision created a relatively thin deformation zone (known...
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Journal Article
Published: 01 July 2015
Journal of the Geological Society (2015) 172 (4): 479-490.
... peridotites and is enveloped by a wide band of mid-ocean ridge basalt (MORB)-like garnet amphibolites ( Fig. 2b ; Němec 1996 ). In this area, the easternmost part of the Moldanubian Zone was thrust over the metamorphosed and deformed western margin of the Brunia microcontinent ( Urban 1992...
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Journal Article
Published: 01 March 2010
Journal of the Geological Society (2010) 167 (2): 329-345.
... between the Moravian zone (metamorphosed Brunia-derived rocks) and the overthrust Moldanubian domain ( Schulmann et al . 2005, 2008 ) is marked by a narrow belt of kyanite-bearing micaschists interpreted as a major shear zone along which the high-grade Moldanubian gneisses and migmatites were...
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Journal Article
Journal: Elements
Published: 01 August 2011
Elements (2011) 7 (4): 253-260.
...) and orogenic middle crust (green and orange), flowed over strong continental crust (Brunia, pink) during late Paleozoic collision. CMP = Central Moldanubian Pluton; OMC = orogenic middle crust; OLC = orogenic lower crust ...
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Journal Article
Published: 01 December 2016
European Journal of Mineralogy (2016) 28 (6): 1047-1057.
... – Bristol Channel-Bray Fault; BM – Bohemian Massif; Br – Brunia; CS – Central Sudetes; EB – Elbe Fault; FMC – French Massif Central; Ga – Ganderia; ISF – Intra-Sudetic Fault; IS – Iapetus suture; MC – Midland craton; MZ – Moldanubian zone; OF – Odra Fault; RM – Rhenish Massif; RS – Rheic suture; ST – Saxo...
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Journal Article
Published: 01 February 2017
Mineralogical Magazine (2017) 81 (1): 15-33.
...; ST, Saxothuringian Unit; M, Moldanubian Unit; B, Brunia Continent; L, Lugian domain. ...
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Book Chapter

Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV1P.12
EISBN: 9781862393929
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Journal Article
Published: 01 September 2013
Journal of the Geological Society (2013) 170 (5): 785-804.
... between Avalonia and Armorica, and two Devonian oceanic and Carboniferous continental sutures (the Teplá suture) located between the Saxothuringian (North Armorica) plate and the southern Gondwana-derived fragments represented by the Teplá–Barrandian–Kraichgau, the Moldanubian and the eastern Brunia...
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Series: European Mineralogical Union Notes in Mineralogy
Published: 01 January 2003
DOI: 10.1180/EMU-notes.5.6
EISBN: 9780903056540
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