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Over the late Holocene highstand, the shoreline at Poverty Bay, NZ migrated 12km seaward, fed by sediment from the Waipaoa river. Paleo-shorelines indicate steadily decelerating progradation, possibly signaling changes in forcing on the Waipaoa Sedimentary System. To isolate the cause of this progradation slowdown we reconstruct late Holocene tectonics and stratigraphy over the Waipaoa coastal plain...
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