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Faulting and folding in the Southern Taranaki Basin constrain the evolution of the New Zealand plate boundary since ~80Ma. Sedimentary rocks up to 8km thick record multiple phases of deformation which have been examined using 2D and 3D seismic reflection data, resulting in fault displacement–time curves and basin-wide isopach maps with temporal resolutions of 5–10Myr and 1–4Myr pre- and post-~23Ma...
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