Collage tectonics in the northeasternmost part of the Variscan Belt: the Sudetes, Bohemian Massif

@article{Aleksandrowski2002CollageTI,
  title={Collage tectonics in the northeasternmost part of the Variscan Belt: the Sudetes, Bohemian Massif},
  author={Paweł Aleksandrowski and Stanisław Mazur},
  journal={Geological Society, London, Special Publications},
  year={2002},
  volume={201},
  pages={237 - 277}
}
Abstract A synthesis of published and new data is used to interpret the Sudetic segment of the Variscan belt as having formed by the accretion of four major and two or three minor terranes. From west to east the major terranes are (1) Lusatia-Izera Terrane, exposing Armorican continental basement reworked by Ordovician plutonism and Late Devonian-Carboniferous collision, showing Saxothuringian affinities; (2) composite Góry Sowie-Kłodzko Terrane characterized by multistage evolution (Silurian… 

Figures from this paper

Geology, tectonic evolution and Late Palaeozoic magmatism of Sudetes–an overview
The Sudetic segment of the Variscides, together with adjacent areas, experienced multistage accretion during successive collisional events that occurred between Middle Devonian and Late Carboniferous
Palaeozoic accretion of Gondwana-derived terranes to the East European Craton: recognition of detached terrane fragments dispersed after collision with promontories
Abstract Recent work in Central Europe, combined with emerging information about basement massifs in SE Europe and NW Turkey, permits a new look at the relationships between crustal blocks abutting
A Variscan continental collision of the West Sudetes and the Brunovistulian terrane: a contribution from structural and metamorphic record of the Stronie Formation, the Orlica-Śnieżnik Dome, SW Poland
Structural, petrological and geochronological data from marbles and mica schists combined with those from highly disputable gneisses and eclogites of the Orlica-Śnieznik Dome (OSD), gave new insights
Correlation of allochthonous terranes and major tectonostratigraphic domains between NW Iberia and the Bohemian Massif, European Variscan belt
The NW Iberian Allochthon and the Teplá-Barrandian and Moldanubian zones represent the internal parts of the Variscan belt in their respective domains. A correlation based on the lithological
Comment on Dörr and Zulauf: Elevator tectonics and orogenic collapse of a Tibetan-style plateau in the European Variscides: the role of the Bohemian shear zone. Int J Earth Sci (Geol Rundsch) (2010) 99: 299–325
  • W. Franke
  • Geology
    International Journal of Earth Sciences
  • 2012
The present comment disproves the tectonic model of a late Devonian/early Carboniferous Tibetan-style collisional plateau in the Teplá-Barrandean (TB) part of the Bohemian Massif, which later
Gneiss protolith ages and tectonic boundaries in the NE part of the Bohemian Massif (Fore-Sudetic Block, SW Poland)
Published geochronological data, petrology, geochemistry and geological context of orthogneisses in the Strzelin and the Stachow complexes (NE-part of the Fore-Sudetic Block), together with
The Variscan Orogen in Poland
The structure and evolution of the Polish part of the Variscan Orogenic Belt is reviewed, based on published data and interpretations. The Sudetic segment of the Variscides, together with adjacent
New insights into the polyphase evolution of the Variscan suture zone: evidence from the Staré Město Belt, NE Bohemian Massif
Abstract Forming a northern continuation of the Moldanubian Thrust Zone, the Staré Město Belt comprises an E-verging thrust stack of three narrow lithotectonic units that exhibit variations in their
Neoproterozoic and Cambro-Ordovician magmatism in the Variscan Kłodzko Metamorphic Complex (West Sudetes, Poland): new insights from U/Pb zircon dating
The Kłodzko Metamorphic Complex (KMC) in the Central Sudetes consists of meta-sedimentary and meta-igneous rocks metamorphosed under greenschist to amphibolite facies conditions. They are comprised
...
1
2
3
4
5
...

References

SHOWING 1-10 OF 325 REFERENCES
The eastern termination of the Variscides: terrane correlation and kinematic evolution
Abstract Analysis of tectonostratigraphic units in the West Sudetes reveals the same geological events as in the areas west of the Elbe Fault Zone: a late Proterozoic (Cadomian) orogenic event,
From Cadomian subduction to Early Palaeozoic rifting: the evolution of Saxo-Thuringia at the margin of Gondwana in the light of single zircon geochronology and basin development (Central European Variscides, Germany)
Abstract Saxo-Thuringia is classified as a tectonostratigraphic terrane belonging to the Armorican Terrane Collage (Cadomia). As a former part of the Avalonian-Cadomian Orogenic Belt, it became
Chronological constraints on the pre-Variscan evolution of the northeastern margin of the Bohemian Massif, Czech Republic
Abstract New single zircon ages enable us to provide an evolutionary scenario for the Neoproterozoic to Cambro-Ordovician tectonic history of part of the easternmost Sudetes along the northeastern
The mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution
  • W. Franke
  • Geology
    Geological Society, London, Special Publications
  • 2000
Abstract The mid-European segment of the Variscides is a tectonic collage consisting of (from north to south): Avalonia, a Silurian-early Devonian magmatic arc, members of the Armorican Terrane
Terranes and terrane boundaries in the Sudetes, northeast Bohemian Massif
In the Sudetes, seven distinct lithostratigraphic terranes exhibit a symmetric distribution. A central region of basinal/oceanic and ophiolitic rocks, the Central Sudetic terrane is bordered,
Crustal‐scale thrusting and extension in the Hercynian Schwarzwald and Vosges, central Europe
The Hercynian outcrop areas in the Schwarzwald of SW Germany and Vosges of easternmost France consist from north to south of three major lithotectonic complexes: very low- to medium grade
The Brunovistulian: Avalonian Precambrian sequence at the eastern end of the Central European Variscides?
Abstract An outline is presented of the present state of research on the Precambrian evolution history of the Brunovistulian, a large (30 000 km2), mainly sediment covered Peri-Gondwana basement
The Tepla(?)/Saxothuringian suture in the Karkonosze–Izera massif, western Sudetes, central European Variscides
Abstract.The southern and eastern Karkonosze–Izera massif (northern Bohemian Massif) exposes blueschist facies rocks and MORB-type magmatic complexes. During Late Devonian to Early Carboniferous
...
1
2
3
4
5
...