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Fig. 1


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Sketch structural map of the southern West African craton (after Milési et al., 1989 and Thiéblemont, 2016). In the original model of Milési et al. (1989), the dextral shear zones (red kinematic arrows) are the latest and related to a regional D3 strike-slip deformation event, whereas sinistral ones (blue kinematic arrows) would be related to a D2 strike-slip regional deformation event.

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