1-20 OF 109 RESULTS FOR

Tepla-Barrandian Unit

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
×Close Modal
Sort by
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.11
EISBN: 9781862394490
... 1994; Beard et al. 1995). The Mariánské Lázně Complex and the adjacent crystalline parts of the Tepla-Barrandian Unit, together with the Saxothuringian Kladska Unit, are often mentioned in the context of correlations with other units bearing serpentinites, amphibolites, eclogites, orthogneisses...
FIGURES | View All (8)
Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.9
EISBN: 9781862396814
... Devonian–early Carboniferous subduction and continental underthrusting of the Saxothuringian Unit beneath the TepláBarrandian Unit resulted in the orogen-perpendicular shortening and growth of an inboard magmatic arc during c. 354–346 Ma; (2) the subduction-driven shortening was replaced by collapse...
FIGURES | View All (10)
Journal Article
Published: 23 October 2019
Journal of the Geological Society (2019) jgs2019-037.
...-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...
FIGURES | View All (10)
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...
FIGURES | View All (9)
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.09
EISBN: 9781862394490
... Abstract The Mariánské-Lázně Complex is a Cambro-Ordovician terrane of oceanic affinity tectonically emplaced between the Saxothuringian Zone and Teplá-Barrandian Unit, NW Czech Republic. It forms a SE-dipping allochthonous body that comprises the largest contiguous exposure of metamorphosed...
FIGURES | View All (10)
Journal Article
Published: 01 October 1999
Journal of the Geological Society (1999) 156 (5): 1003-1020.
... 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. Zulauf G. Schastok...
Journal Article
Published: 01 January 2014
Journal of the Geological Society (2014) 171 (1): 83-95.
... 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 ; Pitra et al . 1999...
FIGURES | View All (5)
Series: Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP405.8
EISBN: 9781862396814
... as deposits from the southern margin of the Rhenohercynian basin. It behaved as a fore-arc region during the late Lower Carboniferous south-directed subduction of the Rhenohercynian basin. The Early Palaeozoic Southern succession is a thin piece of Teplá-Barrandian affinity which originally belonged...
FIGURES | View All (11)
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...
FIGURES | View All (9)
Journal Article
Published: 10 January 2019
Journal of the Geological Society (2019) 176 (3): 492-504.
... Complex ( Fig. 1 ), which is dominated by metabasic rocks. 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...
FIGURES | View All (9)
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.12
EISBN: 9781862394490
...) SE Karkonosze Terrane of affinities to the Saxothuringian oceanic realm, sandwiched betwen the Lusatia-Izera and Góry Sowie-Kłodzko (together with Teplá-Barrandian) terranes, subjected to high pressure-metamorphism and tectonized during Late Devonian-Early Carboniferous convergence. The Kaczawa...
FIGURES | View All (8)
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.08
EISBN: 9781862394278
... 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 regional metamorphism and tectonics, or for early...
FIGURES
Journal Article
Published: 01 December 2016
European Journal of Mineralogy (2016) 28 (6): 1047-1057.
... that the Leszczyniec unit may represent mafic lower crust of the TepláBarrandian upper plate as it comprises numerous felsic rocks and metagabbro with U–Pb zircon age of 494 ± 2 Ma ( Oliver et al. , 1993 ) corresponding to a period of extensive Cambro–Ordovician continental rifting. For now, we favour the former...
FIGURES | View All (8)
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.20
EISBN: 9781862394278
... Abstract The Saxo-Thuringian Belt on the northern flank of the European Variscides resulted from SE-ward subduction of a Cambro-Ordovician rift basin under the TepláBarrandian (Bohemian) margin. It contains ultra-high-pressure (UHP) metamorphic rocks, which are now exposed in different...
FIGURES | View All (10)
Image
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.
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.06
EISBN: 9781862394278
...; Zukalová 1976 ; Cech et al. 1989; Chlúpáč 1994). These stratigraphic constraints suggest deformation in Early or pre-Frasnian time. In the nearby TepláBarrandian Unit, deformation is stratigraphically constrained to Late- to post-Givetian age (Chlúpáč 1993 a, b; Chlúpáč et al. 1998) and Ar—Ar...
FIGURES | View All (6)
Image
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
Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV1P.3
EISBN: 9781862393929
..., Bohemian Massif; M, Moravo-Silesian Unit; MZ, Moldanubian Zone; NAM, North Armorican Massif; S, Sudetes; SXZ, Saxo-Thuringian Zone; TBU, Teplá-Barrandian Unit. The authors are very grateful to J. D. Inglis (Syracuse, USA), T. Brewer (Leicester, UK) and T. McCann (Bonn, Germany) for their critical...
FIGURES | View All (31)
Image
Bar plot of ε Nd  values recalculated to the measured emplacement age of th...
Published: 01 March 2010
), compositions for the following lithologies are plotted: basic–intermediate arc-related Neoproterozoic metavolcanic rocks of the TepláBarrandian Unit ( Pin & Waldhausrová 2007 ; Vokurka et al ., unpublished data), Late Cambrian rift-related volcanic rocks of intermediate–acidic composition ( Pin et al