Most natural examples of transpression zones developed at oblique convergence regime are inherently 3D and
have inclined boundaries. A 3D finite element model with an elasto-plastic rheology is used to investigate the
structural and mechanical evolution of inclined transpression zones in a rock sequence above a frictional basal
detachment. Inelastic constitutive relationships allow permanent strains to develop in response to the applied
loads. FE-modelling results show that oblique convergence is accommodated by discrete deformation at the main
pre-existing inclined faults (¼70 ) and by distributed brittle and ductile deformation at active blocks. Oblique
contraction at the active blocks resulted mainly in layer-parallel shortening, orthogonal to the model outer
boundaries, whereas thickening in the horizontal and vertical directions was accommodated via layer-parallel,
fault strike-parallel extension and up-dip extrusion (i.e., inclined extrusion). Lateral extrusion should have
compensated the rest and/or volume loss took place. Folding and thickening of the mobile backstop produced a
non-cylindrical, asymmetric, bi-vergent anticline where permanent strains developed principally in the steep
forelimb. Secondary, conjugate fault zones also accommodate oblique slip and contribute to uplift. Displacement
vectors within the transpression zone are rotated counter-clockwise (ca. 20 –30 ) with respect to vectors in the
fixed backstop. Areas with higher rotation values seem to correlate with those showing higher ellipticity values.
The presence of pre-existing faults favored strain partitioning from the onset of deformation. FE-modelling results
compared with analytical, natural example, and analogue modelling results show that our mechanical
modelling can overall match inclined transpression zones geometry that present different modes of strain partitioning
and localisation.
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