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Tepla-Barrandian Unit

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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.11
EISBN: 9781862394490
... Abstract Bodies of coronitic metagabbro occur in the SW Mariánské Lázně Complex (MLC) and the adjacent Teplá Crystalline Unit (TCU) on the western margin of the Teplá-Barrandian Unit (TBU), Bohemian Massif. The characteristic structural, geochemical, petrographic, and metamorphic features...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.9
EISBN: 9781862396814
... The upper-crustal TepláBarrandian Unit in the centre of the Bohemian Massif (Fig. 2 ) occupies the hanging-wall position with respect to the neighbouring Saxothuringian and Moldanubian units and is thus the overriding plate for all the hypothetical subduction zones. Moreover, a large central...
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Journal Article
Published: 23 October 2019
Journal of the Geological Society (2020) 177 (2): 325–341.
...-alkaline arc-like geochemical signature of the orthogneisses is interpreted as inherited from the recycled Cadomian metasedimentary source and both the magmatic and metasedimentary rocks are correlated with similar occurrences in the adjacent Moldanubicum and TepláBarrandian Unit. The Late Cambrian–Early...
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Journal Article
Published: 01 June 2012
European Journal of Mineralogy (2012) 24 (3): 483–497.
...Shah Wali Faryad Abstract The Mariánské-Lázně Complex is a Cambro-Ordovician terrane with metabasites of oceanic-crust affinity and tectonically emplaced between the Saxothuringian Zone and the Teplá-Barrandian Unit (western part of the Bohemian Massif). It is formed by amphibolite (retrogressed...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.09
EISBN: 9781862394490
... The Teplá-Barrandian Unit (Perunica micro-continent of Havlifček et al. 1994) features a well preserved section of the Cadomian Orogen in Central Europe and is considered to have behaved as a separate microplate within the ATA in early Palaeozoic times ( Franke 1989 ; Matte et al...
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Journal Article
Published: 01 September 1999
Journal of the Geological Society (1999) 156 (5): 1003–1020.
... Journal of Geophysics 1988 62 69 101 Dörr, W., Fiala, J., Philippe, S., Vejnar, Z. & Zulauf, G. 1995. Cadomian vs. Variscan imprints in the Tepla-Barrandian unit. Part A: U-Pb ages of the pre-Variscan granitoids. 4. Kolloquium “Orogene Prozesse”, 29.–30.3. 1995, Jena. Dörr W...
Journal Article
Published: 23 October 2013
Journal of the Geological Society (2014) 171 (1): 83–95.
...-sedimentary sequences ( Drost et al . 2007 ; Hajná et al . 2011 , 2013 ) in the NW. The character of juxtaposition of these units has been widely discussed and the models either propose a completely independent character of the TepláBarrandian block in the Bohemian Massif assembly (e.g. Rajlich 1993...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.8
EISBN: 9781862396814
... comprise sediments of Rhenohercynian affinity separated from Teplá-Barrandian metasediments by a Lower Carboniferous magmatic arc. The latter is correlated with the Mid-German Crystalline Rise, and is ascribed to the south-directed subduction of the Rhenohercynian Basin. The Saxothuringian–Moldanubian...
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Series: GSA Special Papers
Published: 01 January 1989
DOI: 10.1130/SPE230-p67
...; Tepla/Barrandian microplate; Barrandian/Moldanubian basin, which is possibly continued westward in the Southern Vosges/Black Forest basin; Vindelician microplate; Massif Central/Western Alps narrow ocean; and southern Europe, possibly separated by an additional basin from Gondwanaland. Closure of all...
Journal Article
Published: 01 March 2010
Journal of the Geological Society (2010) 167 (2): 347–360.
...Vojtĕch Janoušek; Bettina A. Wiegand; Jiří Žák Abstract: The Variscan Central Bohemian Plutonic Complex crops out between the upper-crustal TepláBarrandian and the high-grade Moldanubian units (Bohemian Massif). Much of the complex is made up of calc-alkaline plutonic rocks: (1) the geochemically...
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Journal Article
Published: 10 January 2019
Journal of the Geological Society (2019) 176 (3): 492–504.
.... This unit has been interpreted by Mazur & Aleksandrowski (2001) as a remnant of the floor of the Saxothuringian Ocean attached to the upper (TepláBarrandian) plate in the early stages of the subduction process, as it does not show signs of high-pressure metamorphism ( Kryza & Mazur 1995...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.12
EISBN: 9781862394490
... Central and Armorican Massif in France as well as with the Teplá-Barrandian Terrane that extends well beyond the Sudetes into the central Bohemian Massif. (5) The Teplá-Barrandian Terrane, in its Sudetic segment, is interpreted here to incorporate the Nové Město Belt, Zabŕeh Unit and the SW part...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.08
EISBN: 9781862394278
.... ( 1998 ), Zulauf al. (1999). Figure 3 illustrates that the recorded Cadomian events in the Brunovistulian are significantly distinct from those in the TepláBarrandian Unit and the Saxothuringian. A first important difference is that the Brunovistulian does not show evidence for Eocambrian...
FIGURES
Journal Article
Published: 01 December 2016
European Journal of Mineralogy (2016) 28 (6): 1047–1057.
... from a subduction–exhumation channel. We postulate that the Kopina blueschists were formed in a subduction system developed along the eastern termination of the Saxothuringian Ocean and operating beneath the TepláBarrandian upper plate. When combined with previous data on continental crust affinity...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.20
EISBN: 9781862394278
... The Saxo-Thuringian Belt is situated on the northern flank of the European Variscan Orogen. It represents the hinterland of the Rheno-Hercynian Orogen adjacent to the NW, and, at the same time, the foreland to the TepláBarrandian leading edge impinging from the SE (see foldout map...
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Comparison of zircon ages from the meta-igneous rocks of the Kouřim <b>Unit</b> (K...
Published: 23 October 2019
Fig. 6. Comparison of zircon ages from the meta-igneous rocks of the Kouřim Unit (KU) and their host rocks (this study) with published detrital zircon ages from the Moldanubicum ( Košler et al. 2014 ; Žák & Sláma 2017 ; Bukovská et al. 2019 ) and TepláBarrandian ( Drost et al. 2011
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Geological sketch of the Kaczawa structural <b>unit</b> (based on  Kryza and Muszy...
Published: 01 February 2011
Fault Zone, ISF – Intra-Sudetic Fault Zone, MGCR – Mid-German Crystalline Rise, MO – Moldanubian Zone, MS – Moravo-Silesian Zone, NP – Northern Phyllite Zone, OFZ – Odra Fault Zone, RH – Rheno-Hercynian Zone, ST – Saxo-Thuringian Zone, TB – Tepla-Barrandian Zone.
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Geotectonic diagrams for the rocks of the Kouřim <b>Unit</b> and published data fr...
Published: 23 October 2019
Fig. 7. Geotectonic diagrams for the rocks of the Kouřim Unit and published data from the Moldanubicum ( René 2006 ) and TepláBarrandian ( Drost et al. 2007 ; Fiala et al. 2014 ) (meta-)sedimentary rocks (semi-transparent symbols). ( a ) Binary plot CaO/(MgO + FeO T ) v. Al 2 O 3 /(MgO
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.06
EISBN: 9781862394278
... the Prague Syncline of the TepláBarrandian Unit (Chlupáč 1994 ). The Proterozoicx and Palaeozoic sequence of Železné hory ranges up-section into palaeontologically dated rocks of Silurian age, and most probably into Early Devonian time. Devonian limestone pebbles in Permian conglomerates south of Mlada...
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Tectonic map of Bohemian Massif. Lower plate tectonic <b>units</b> are autochthono...
in > Geology
Published: 01 April 2014
Figure 1. Tectonic map of Bohemian Massif. Lower plate tectonic units are autochthonous (Saxo-Thuringian domain, dark green) or allochthonous (Saxo-Thuringian and Moldanubian domains, light green-yellow). Upper plate tectonic units are represented by supracrustal rocks (Teplá-Barrandian domain