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A major Mesoproterozoic magmatic—extensional event in the Vestfold Hills started with normal faulting, followed by lamprophyric dyke emplacement and by two distinct episodes of FRT dyke emplacement at 13 Ma.A consistent direction of the stress field during this event suggests control of a linear belt of crustal uplift.The Vestfold Hills formed part of a relatively stable craton, peripheral to the mobile belt that was formed during these events.
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The geometry and orientation of 2240 Ma HMT dykes imply a low deviatoric extensional stress field, inconsistent with a mantle plume origin for magmatism.