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Original Article |
1 1Ecole et Observatoire des Sciences de la Terre, UMR 7516 of CNRS, 5 Rue René Descartes, 67084 Strasbourg Cedex, France (e-mail: JeanBernard.Edel@eost.u-strasbg.fr)
2 2Institute of Petrology and Structural Geology, Univerzita Karlova, Albertov 6, Praha 2, Czech Republic
New palaeomagnetic data from Lower Carboniferous granitoids of the orogenic root of the eastern Variscan belt (Moldanubian domain) show a polyphase palaeomagnetic record. Comparison of the data with existing palaeomagnetic measurements from Lower Palaeozoic sequences of the Bohemian Massif demonstrates a Carboniferous remagnetization of these latter units. All the data presented suggest that the Saxothuringian basement, the Moldanubian orogenic root system as well as the eastern Neoproterozoic Brunovistulian basement were already assembled during the Early Carboniferous. The whole Variscan belt subsequently rotated in a clockwise direction during MidLate Carboniferous times. Structural and geochronological data indicate that this rotation was accompanied by large-scale dextral wrenching along NWSE-trending lithospheric faults. In a first stage, the blocks limited by wrench-faults rotated anticlockwise in bookshelf manner. The data presented rule out the existing model of oroclinal bending of the Rhenohercynian zone at the eastern termination of the Variscan belt.
Key Words: palaeomagnetism Carboniferous Bohemian massif rotation wrenching
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