The Variscan metamorphic and structural evolution of the Maures-Tanneron massif is divided in two main post-collisional phases: (1) a MP-MT regional gradient is developed during nappe-piling process between 350 and 320 Ma, followed by (2) LP-HT regional gradient coeval with doming between 320 and 300 Ma. During this late phase, the tectonic...
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May 2009 (v1)Journal articleUploaded on: December 4, 2022
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2008 (v1)Journal article
Journal of the Geological Society of London, v. 165, n. 2, p. 467-478, 2008. http://dx.doi.org/10.1144/0016-76492007-045
Uploaded on: December 3, 2022 -
2010 (v1)Journal article
Detailed 40Ar/39Ar geochronology on single grains of muscovite was performed in the Variscan Tanneron Massif (SE France) to determine the precise timing of the post-collisional exhumation processes. Thirty-two plateau ages, obtained on metamorphic and magmatic rocks sampled along an east–west transect through the massif, vary from 302 ± 2 to...
Uploaded on: December 3, 2022