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Structure, texture, and physical properties of accretionary prism sediments and fluid flow near the splay fault zone in the Nankai Trough, off Kii Peninsula
潮岬海底谷に露出する南海トラフ分岐断層付近の付加体堆積物の構造・組織・物性と流体移動
2010
Chishitsugaku zasshi
潮岬海底谷に露出する南海トラフ分岐断層付近の付加体堆積物の構造・組織・物性と流体移動
Shionomisaki Canyon, off Kii Peninsula, SW Japan, cuts through fi ve E-W-trending ridges developed in the Nankai accretionary prism. Using the submersible SHINKAI , we investigated outcrops along the eastern canyon wall in the landward-most ridge. Four dives yielded information on lateral variations in the structure, texture, and physical properties of sediments along the splay fault zone in the accretionary prism. The ridge itself is disrupted by E-W-trending gullies that continue to
doi:10.5575/geosoc.116.637
fatcat:akn3f3cafzectkye7vbyqa2ug4