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3-D numerical modelling of the influence of pre-existing faults and boundary conditions on the distribution of deformation: Example of North-Western Ghana
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We have used the Underworld code to test different orientations of a system of branched crustal scale strike-slip faults.

The orientations of faults control the evolution of relief and localized deformation.

We have modelled topographic evolution using three different surface boundary conditions.

We have reconstructed the Bole-Bulenga terrane in North-Western Ghana (around 2.20–2.10 Ga).

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