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Geomorphologic Controls on the Evolution of Submarine Channels in the Clifdenian-Tongaporutuan Interval of the Southern Taranaki Basin, offshore New Zealand
doi.org/10.31223/X5V36G ;Architecture;SeismicAttributes;PalaeoenvironmentReconstruction;Miocene;TaranakiBasin;SubmarineChannels;Climate;TurbidityCurrent;Sea-level

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