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Volume 4, issue 1
Solid Earth, 4, 135–152, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Solid Earth, 4, 135–152, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 Apr 2013

Research article | 17 Apr 2013

Strain localisation in mechanically layered rocks beneath detachment zones: insights from numerical modelling

L. Le Pourhiet2,1, B. Huet3, L. Labrousse2,1, K. Yao5, P. Agard2,1, and L. Jolivet4 L. Le Pourhiet et al.
  • 1UPMC Univ Paris 06, UMR 7193, ISTEP, 75005, Paris, France
  • 2CNRS, UMR 7193, ISTEP, 75005, Paris, France
  • 3Department for Geodynamics and Sedimentology, University of Vienna, Althanstrasse 14 1090 Vienna, Austria
  • 4ISTO, UMR CNRS 6113, Université d'Orléans, Campus CNRS, 1A rue de La Férollerie, 45071 Orlans Cedex, France
  • 5Mines ParisTech, Centre de Géosciences, 35 rue Saint Honoré, 77305 Fontainebleau, France

Abstract. We have designed a series of fully dynamic numerical simulations aimed at assessing how the orientation of mechanical layering in rocks controls the orientation of shear bands and the depth of penetration of strain in the footwall of detachment zones. Two parametric studies are presented.

In the first one, the influence of stratification orientation on the occurrence and mode of strain localisation is tested by varying initial dip of inherited layering in the footwall with regard to the orientation of simple shear applied at the rigid boundary simulating a rigid hanging wall, all scaling and rheological parameter kept constant. It appears that when Mohr–Coulomb plasticity is being used, shear bands are found to localise only when the layering is being stretched. This corresponds to early deformational stages for inital layering dipping in the same direction as the shear is applied, and to later stages for intial layering dipping towards the opposite direction of shear. In all the cases, localisation of the strain after only γ=1 requires plastic yielding to be activated in the strong layer.

The second parametric study shows that results are length-scale independent and that orientation of shear bands is not sensitive to the viscosity contrast or the strain rate. However, decreasing or increasing strain rate is shown to reduce the capacity of the shear zone to localise strain. In the later case, the strain pattern resembles a mylonitic band but the rheology is shown to be effectively linear.

Based on the results, a conceptual model for strain localisation under detachment faults is presented. In the early stages, strain localisation occurs at slow rates by viscous shear instabilities but as the layered media is exhumed, the temperature drops and the strong layers start yielding plastically, forming shear bands and localising strain at the top of the shear zone. Once strain localisation has occured, the deformation in the shear band becomes extremely penetrative but the strength cannot drop since the shear zone has a finite thickness.

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