Abstract
In the southern French Massif Central, the Rocles leucogranite of Variscan age consists of three petrographic facies; textural analysis shows that they experienced the same subsolidus deformation. New chemical U-Th-Pb dating on monazite yielded 324 ± 4 Ma and 325 ± 5 Ma ages for muscovite-rich and biotite-rich facies respectively. AMS-study results agree with petrostructural observations. The magnetic planar and linear fabrics, which correspond to the preferred orientation of biotite and muscovite, are consistent with the foliation and lineation defined by the preferred mineral orientation. This fabric developed during pluton emplacement. The accordance of this granite foliation with that observed in the host rock, suggests that the Rocles pluton is a laccolith, but its present geometry resulted from post-emplacement southward tilting due to the uplift of the Late Carboniferous Velay dome. Restoration of the primary geometry of the pluton and its country-rocks to a flat-lying attitude places the granite lineation close to the trend measured in other plutons of the area. This restoration further supports the interpretation of the Rocles laccolith as a pluton emplaced along a tectonic contact reactivated during the late-orogenic collapse of the Variscan Belt.
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Acknowledgements
This study has been supported by P. Rossi and the “Carte Géologique de la France” programme at BRGM (French Geological Survey). The Conseil Régional du Centre is acknowledged for financial support. The authors would like to acknowledge the Institut des Sciences de la Terre d’Orléans (ISTO) for providing analytical facilities.
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Be Mezeme, E., Faure, M., Chen, Y. et al. Structural, AMS and geochronological study of a laccolith emplaced during Late Variscan orogenic extension: the Rocles pluton (SE French Massif Central). Int J Earth Sci (Geol Rundsch) 96, 215–228 (2007). https://doi.org/10.1007/s00531-006-0098-2
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DOI: https://doi.org/10.1007/s00531-006-0098-2