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Timing of dextral strike-slip processes and basement exhumation in the Elbe Zone (Saxo-Thuringian Zone): the final pulse of the Variscan Orogeny in the Bohemian Massif constrained by LA-SF-ICP-MS U–Pb zircon data

By
M. Hofmann
M. Hofmann
Staatliche Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Königsbrücker Landstraße 159, D-01109 Dresden, Germany
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U. Linnemann
U. Linnemann
Staatliche Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Königsbrücker Landstraße 159, D-01109 Dresden, Germany
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A. Gerdes
A. Gerdes
Institut für Geowissenschaften, Johann Wolfgang Goethe-Universität, FE Mineralogie, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
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B. Ullrich
B. Ullrich
TU Dresden, Institut für Geotechnik, Lehrstuhl für Angewandte Geologie, Neuffer-Bau, Helmholtzstraße 10, D-01069 Dresden, Germany
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M. Schauer
M. Schauer
Am Hexenberg 8, 09224 Grüna, Germany
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Published:
January 01, 2009

Abstract

The final pulse of the Variscan Orogeny in the northern Bohemian Massif (Saxo-Thuringian Zone) is related to the closure of the Rheic Ocean, which resulted in subduction-related D1-deformation followed by dextral strike-slip activity (D2-deformation, the Elbe Zone). Taken together, these deformation events reflect the amalgamation of Pangaea in central Europe. Lateral extrusion of high-grade metamorphosed rocks from an allochthonous domain (Saxonian Granulitgebirge) and the top–NW-directed transport of these domains (Erzgebirge nappe complex, Saxonian Granulitgebirge) are responsible for these dextral strike-slip movements. Geochronological data presented herein, together with published data, allow the timing of the final pulse of the Variscan Orogeny and related plutonic, volcano-sedimentary and tectonic processes. Marine sedimentation lasted at least until the Tournaisian (357 Ma). Onset of Variscan strike-slip along the Elbe Zone is assumed to be coeval with the beginning of the top–NW-directed lateral extrusion of the Saxonian Granulitgebirge at 342 Ma (D2-deformation). The sigmoidal shape of the Meissen Massif indicates that strike-slip activity was coexistent with intrusion of the pluton at c. 334 Ma into the schist belt of the Elbe Zone. In contrast, the intrusion of the Markersbach Granite provides a minimum age of c. 327 Ma for the termination of D2 strike-slip activity, because this undeformed pluton cross-cuts all strike-slip related tectonic structures. Geochronological data of an ash bed from the Permo-Carboniferous Döhlen Basin show clearly that post-orogenic sedimentation of Variscan molasse in that area was already active at 305 Ma. This pull-apart basin is a local example of regional Permo-Carboniferous extension within Pangaea. The uplift and denudation of the Variscan basement in the Saxo-Thuringian Zone occurred between c. 327–305 Ma.

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Contents

Geological Society, London, Special Publications

Ancient Orogens and Modern Analogues

J. B. Murphy
J. B. Murphy
St Francis Xavier University, Canada
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J. D. Keppie
J. D. Keppie
Universidad Nacional Autonoma de Mexico, Mexico
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A. J. Hynes
A. J. Hynes
McGill University, Canada
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Geological Society of London
Volume
327
ISBN electronic:
9781862395756
Publication date:
January 01, 2009

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