Structure of Late Variscan Millevaches Leucogranite Massif in the French Massif Central: AMS and Gravity Modelling Results
University of Plymouth PEARL https://pearl.plymouth.ac.uk 01 University of Plymouth Research Outputs University of Plymouth Research Outputs 2006-01 Structure of late Variscan Millevaches leucogranite massif in the French Massif Central: AMS and gravity modelling results Gebelin, A http://hdl.handle.net/10026.1/8625 10.1016/j.jsg.2005.05.021 Journal of Structural Geology Elsevier BV All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Journal of Structural Geology 28 (2006) 148–169 www.elsevier.com/locate/jsg Structure of late Variscan Millevaches leucogranite massif in the French Massif Central: AMS and gravity modelling results Aude Ge´belina,*, Guillaume Marteletb, Yan Chenc, Maurice Brunela, Michel Faurec aLaboratoire Dynamique de la Lithosphe`re, Universite´ Montpellier II, CC060, Place E. Bataillon, 34095 cedex 5, Montpellier, France bBRGM, BP 6009, 45060 Orle´ans cedex, France cInstitut des Sciences de la Terre d’Orle´ans, UMR 6113, Universite´ d’Orle´ans, BP 6759, 45067 Orle´ans cedex 2, France Received 15 May 2004; received in revised form 20 May 2005; accepted 24 May 2005 Available online 28 November 2005 Abstract In the Limousin area, Variscan leucogranitic plutons are spatially associated with normal faults and major strike-slip shear zones that are a continuation of the South Armorican shear zone.
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