K
Ken Ikehara
Researcher at National Institute of Advanced Industrial Science and Technology
Publications - 198
Citations - 3735
Ken Ikehara is an academic researcher from National Institute of Advanced Industrial Science and Technology. The author has contributed to research in topics: Trench & Holocene. The author has an hindex of 30, co-authored 189 publications receiving 3158 citations.
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The 2011 Tohoku-oki tsunami-induced sediment remobilization on the Sendai shelf, Japan, from a comparison of pre- and post-tsunami surface sediments.
TL;DR: In this article, the surface sediments before and after the 2011 Tohoku-oki tsunami on the Sendai shelf were compared and it was shown that both sandy and muddy sediments were significantly reworked on the shelf.
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Distribution of mollusc shells in the Sea of Okhotsk off Hokkaido
TL;DR: In this article, a list of marine molluscs in the Sea of Okhotsk, off Hokkaido, at the Institute for Marine Resources and Environment, Geological Survey of Japan/AIST (National Institute of Advanced Industrial Science and Technology).
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Millennial-scale changes of surface and bottom water conditions in the northwestern Pacific during the last deglaciation
TL;DR: In this article, changes in water column conditions in the northwestern Pacific during the last 23-ka were reconstructed using geochemical and isotope proxies and redox elemental compositions along with published data (alkenone sea surface temperature and benthic foraminiferal fauna) at core GH02-1030.
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Stratigraphy of deep-sea marine sediment using paleomagnetic secular variation: Refined dating of turbidite relating to giant earthquake in Japan Trench
TL;DR: In this paper, the ages of turbidite units regarded as induced by the Jogan earthquake were inferred from two sedimentary cores that closely approximate its documented age using the PSV master curve.
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Variations in sediment lithology of submarine flood deposits on the slope off Kumano River, Japan
TL;DR: In this article, the authors examined the occurrence of flood deposits along the slope off the mouth of Kumano River in four surface sediment cores collected around 2 months after the 2011 flood.