1-20 OF 91 RESULTS FOR

Tepla-Barrandian Terrane

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
... of the Teplá Barrandian terrane with Saxothuringia (e) in which the rocks of the MLC and TCU were thrust to the NW over the Saxothuringian para-autochthon. The accompanying metamorphic event reached upper amphibolite facies. The thermally relaxed rocks cooled rapidly, and pre-existing thrust planes were re...
FIGURES | View All (8)
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)
Journal Article
Published: 01 October 1999
Journal of the Geological Society (1999) 156 (5): 1003-1020.
...PAVEL PITRA; JEAN-PIERRE BURG; MICHEL GUIRAUD Abstract In the Variscan Bohemian Massif (Czech Republic), no agreement has been reached on the nature of the relationship between the Teplá-Barrandian and the Moldanubian terranes. However, the Teplá-Barrandian is interpreted as a central segment...
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: 01 January 2014
Journal of the Geological Society (2014) 171 (1): 83-95.
... in the northeastern part of the Bohemian Massif . Journal of Geosciences , 55 , 299 – 319 . Pitra P. Burg J.P. Guiraud M. 1999 . Late Variscan strike-slip tectonics between the TepláBarrandian and Moldanubian terranes (Czech Bohemian Massif): petrostructural evidence . Journal...
FIGURES | View All (5)
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.08
EISBN: 9781862394278
... to mid-Cambrian granitoid plutonism or related volcanism, whereas Dörr et al. ( 1998 , in prep.) have pointed out that these two events are widely recorded throughout the Armorican terrane assembly, from central Europe over Brittany to Spain. In the case of the TepláBarrandian Unit, Zulauf et al...
FIGURES
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 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: 10 January 2019
Journal of the Geological Society (2019) 176 (3): 492-504.
... was partly subducted and partly relaminated underneath the overriding TepláBarrandian Domain. However, our data, as well as data from mafic high-pressure rocks in the southern part of the Saxothuringian Domain, suggest that the initial collision was probably caused by the arrival of a smaller crustal block...
FIGURES | View All (9)
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...
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
... a ). These findings suggest a regime of (gross) SE-ward subduction of the Saxo-Thuringian passive margin under the NW margin of the TepláBarrandian (Bohemian terrane), at least partly combined with dextral transpression (Franke this volume). Rocks with similar metamorphic ages occur to the SE...
FIGURES | View All (10)
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)
Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP297.17
EISBN: 9781862395459
... shown to have close affinities with Cadomia and West Africa (Fig.  12 ), whereas the Moravo-Silesian zone (Brunovistulian) has Avalonian affinities ( Zulauf et al. 1999 ; Finger et al. 2000 ; Linnemann & Romer 2002 ; Linnemann et al. 2004 ). In the Moldanubian zone, the TepláBarrandian...
FIGURES | View All (18)
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.05
EISBN: 9781862394278
.... this volume). The TB has been rotated counterclockwise through at least 140° since the Silurian, and before the onset of collisional deformation in late Devonian time (Tait et al. 1994 , this volume). The TepláBarrandian and the high-grade metamorphic rocks adjacent to the SE have been summarized...
FIGURES | View All (9)
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)
Series: Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.19
EISBN: 9781862394070
... et al . 1988 ; Bröcker et al . 1998 ; Timmermann et al . 2000 ) and appears to be contemporary with HP-LT metamorphism along the contact zone of the Saxo-Thuringian and Teplá-Barrandian blocks between 380 and 365 Ma. Further west, recently obtained mid- to late Devonian dates...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.08
EISBN: 9781862394490
..., Iberia) that lie south of the southeastern active margin of the Rheno-Hercynian Zone (Mid-German Crystalline High) and form the inner part of the orogen. The root of the Moldanubian Zone is of uncertain origin, whereas relicts of the Cadomian Orogen are preserved in the Teplá-Barrandian Unit and areas...
FIGURES | View All (6)
Image
Peri-Gondwanan <b>terranes</b> of southern and central Europe (modified from  Linn...
Published: 01 December 2016
-Thuringia; STS – Saxo-Thuringian suture; TB – TepláBarrandian zone; TS – Thor Suture; TTZ – Teisseyre–Tornquist zone. (Online version in colour)
Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP325.5
EISBN: 9781862395732
..., but that it was possibly still part of a separate plate; that is, comparable with the current relationship between parts of California and the rest of the North American continent (Fig.  2 ). The TepláBarrandian area in the Czech Republic, incorporating the classical geological successions of the Prague Basin, might...
FIGURES