southward propagation of deformation from the orogen created a number of emergent thrusts and thrust related anticlines along the margins of the basin and within the basin itself. The effect that the growth of these kilometre scale structures had on the coeval marine depositional systems is the focus of this work. Although the effects that uplifting intrabasinal structures have on fluvial systems and the effects that basin margin structures have on marine systems are well covered in the literature
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