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A model is presented that combines the traditional approach to transpression with the thin viscous sheet approx- imation of the lithosphere, to study deformation in front of an obliquely colliding indenter. The model produces a zone dominated by lateral simple shear (orogen parallel transcur- rent movements) close to the indenter and a zone of dom- inant pure shear (orogen perpendicular pure shear/thrusting regions) further away from the indenting boundary. The rel- ative width of simple shear dominated zone with respect to the more distant pure shear domain in terms of the angle of convergence is discussed. The possibility of development of transcurrent faults in front of an indenting plate is enhanced by the reactivation of fabric anisotropy created progressively during indentation.

Strain partitioning in front of an obliquely convergent indenter