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Flow path of the 1993 Hokkaido-Nansei-oki earthquake seismoturbidite, southern margin of the Japan sea north basin, inferred from anisotropy of magnetic susceptibility
Authors:A L Abdeldayem  K Ikehara  T Yamazaki
Institution:Geology Department, Faculty of Science, Tanta University, Tanta 31527,;Egypt. E-mail: MRE, Geological Survey of Japan, AIST, Higashi 1-1-1,;Tsukuba 305-8567, Japan
Abstract:
Keywords:AMS  deep-sea sediments  Japan sea  palaeocurrent  seismoturbidite
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