Search Results1-8 of  8

  • KUBOSHIMA Koji ID: 9000006340666

    Grad. Scn. Sci. & Tech., Niigata Univ. (2007 from CiNii)

    Articles in CiNii:4

    • P-72 Color analysis of the fault gouges in the western Tottori Prefecture, Japan (2006)
    • P-99 Brittle fault rocks along the Shibata-Koide Tectonic Line, Mid-Niigata prefecture (2006)
    • P-100 Geological study of low activity faults in the western part of the Tottori prefecture, Japan (2006)
  • KUBOSHIMA Koji ID: 9000347165877

    Grad. Sch. Sci. & Tech., Niigata Univ. (2007 from CiNii)

    Articles in CiNii:1

    • (U-5)Directions of strong ground motions accompanying the Niigataken Chuetsu-oki Earthquake in 2007, Japan. (2007)
  • Koji Kuboshima ID: 9000347166901

    Japan Atomic Energy Agency (2014 from CiNii)

    Articles in CiNii:1

    • Study on influence of fault activity to geological environment, case study at the Mizunami Underground Research Laboratory (2014)
  • Kuboshima Koji ID: 9000006340682

    Niigata University (2006 from CiNii)

    Articles in CiNii:1

    • P-99 Brittle fault rocks along the Shibata-Koide Tectonic Line, Mid-Niigata prefecture (2006)
  • Kuboshima Koji ID: 9000258410533

    Grad.Scn.Sci.&Tech.,Niigata Univ. (2007 from CiNii)

    Articles in CiNii:1

    • Geological study of low activity faults in the western part of the Tottori prefecture,Japan. Defference of forming and changing and environments of crush zone of fault core vs damage zone and fault core vs another fault core . (2007)
  • Kuboshima Koji ID: 9000258417521

    Articles in CiNii:1

    • Fault rocks analyses of low activity faults in the western part of the Tottori prefecture (2011)
  • Kuboshima Koji ID: 9000347082543

    Japan Atomic Energy Agency (2012 from CiNii)

    Articles in CiNii:1

    • The process of fault rocks growth in the Mizunami Underground Research Laboratory site area. (2012)
  • Kuboshima Koji ID: 9000347136185

    Japan Atomic Energy Agency (2013 from CiNii)

    Articles in CiNii:1

    • Process of fault growth in and around the Mizunami Underground Research Laboratory site based on texture and mineral composition of fault rocks (2013)
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