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Bulletin de la Societe Geologique de France; May-June 2009; v. 180; no. 3; p. 283-292; DOI: 10.2113/gssgfbull.180.3.283
© 2009 Societe Geologique de France
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Monazite U-Th/Pb chemical dating of the Early Carboniferous syn-kinematic MP/MT metamorphism in the Variscan French Massif Central

Jérémie Melleton1,2, Michel Faure1 and Alain Cocherie2

1 Institut des Sciences de la Terre d’Orléans (ISTO), UMR CNRS 6113, 45067 Orléans cedex 2, France. j.melleton{at}free.fr
2 Bureau de Recherches Géologiques et Minières (BRGM), BP 36009, 45060 Orléans Cedex 2, France.

In situ U-Th-Pb geochronology on monazite using Electron Probe Micro Analyser, constrained by structural and textural observations, has been performed on four samples from the Limousin area (northwest part of the French Massif Central) in order to date the syn-kinematic MP/MT metamorphism related to the top-to-the-NW shearing that deformed the stack of nappes in this zone of the Variscan belt. All the analyzed samples lead to a mean age at 360 ± 4 Ma. The close range of ages obtained during this study (360 Ma) and with the previous 40Ar-39Ar ones (360–350 Ma) suggests fast processes of cooling and exhumation during the Early Carboniferous in internal zones of the Variscan belt. The geodynamic significance of this Early Carboniferous event is discussed at the scale of the Ibero-Armorican orocline.

Key Words: Monazite U-Th/Pb chemical dating • French Massif Central • Limousin • Variscan belt







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