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  • Pierre Lanari, Stéphane Guillot, +4 authors Olivier Beyssac
  • Geology
  • 2012 (First Published: 1 May 2012)
  • Abstract The study of continental subduction processes requires detailed Pressure Temperature ( P – T ) paths to understand the kinematic of burial and exhumation of continental units. In the FrenchContinue Reading
    Abstract The Mertz shear zone (MSZ) is a lithospheric scale structure that recorded mid-crustal deformation during the 1.7 Ga orogeny. We performed a microstructural and crystallographic preferredContinue Reading
    We present new analogue modelling results of crustal thrust-systems in which a deformable (brittle) hanging wall is assumed to endure passive internal deformation during thrusting, i.e. exclusivelyContinue Reading