The latest event at the eastern part of the Atotsugawa fault, inferred from the outcrops at Sako, Hida City, central Japan

  • Doke Ryosuke
    Graduate School of Science and Engineering for Education, University of Toyama
  • Takeuchi Akira
    Graduate School of Science and Engineering for Research, University of Toyama

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Other Title
  • 岐阜県飛騨市神岡町佐古における断層露頭と跡津川断層東部の最新活動
  • ギフケン ヒダシ カミオカマチ サコ ニ オケル ダンソウ ロトウ ト アトツガワ ダンソウ トウブ ノ サイシン カツドウ

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Abstract

We discovered two fault outcrops at the eastern part of the Atotsugawa fault in Sako, Hida City. Radiocarbon dating of the samples from the fluvial strata of the outcrops indicates 100±30 yrs BP and 140±30 yrs BP. Since the fault plane clearly cut the strata, the latest faulting event occurred after these ages. This event is correlative with the AD1858 Hietsu earthquake, on the basis of the historical record of earthquakes in Japan. From the results of previous studies and this study, it is considered that the faulting occurred in all the section of the Atotsugawa fault during the latest event.<BR>Because the timing and interval of the faulting events which occurred less than 10,000 years ago are almost compatible between the western and eastern parts of the Atotsugawa fault, it is probable that the older faulting events also occurred at once in all the parts of the fault.

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