Offshore Fault-related Fold along the Eastern Marginal Zone of Ishikari Lowland, Hokkaido, Japan

DOI Web Site 15 References
  • OGAMI Takashi
    Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology
  • ABE Shintaro
    Research Division for Earthquake and Disaster Mitigation, Association for the Development of Earthquake Prediction
  • YAGI Masatoshi
    GEOSYS, Inc.
  • UCHIDA Yasuto
    Research Institute of Energy, Environment and Geology, Hokkaido Research Organization
  • NISHINA Kenji
    Research Institute of Energy, Environment and Geology, Hokkaido Research Organization
  • MUKAIYAMA Kenjiro
    Kawasaki Geological Engineering Co., Ltd.
  • SAKAMOTO Junya
    Kawasaki Geological Engineering Co., Ltd.
  • ARAI Ryoyu
    Kawasaki Geological Engineering Co., Ltd.

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Other Title
  • 石狩低地東縁断層帯の海域延長部に発達する断層関連褶曲

Abstract

<p>Distributions, characteristics, and activities of offshore fault-related folds which comprise the southern part of the Eastern Boundary Fault Zone of Ishikari Lowland (EBFIL) are clarified by conducting a high-resolution multi-channel seismic reflection survey. To determine termination point of the fault zone, we placed seven survey lines perpendicular to the fault-related folds with a total line length of 107.5 km. We choose a compact water gun (15 cubic inch) as the seismic source to obtain high-resolution imagery of the Late Quaternary and investigate activity of the fault zone. Based on seismic facies, we distinguished packages of offshore sediment (unit 2, 3 and 4, in descending order), which separated by downlap surfaces and correlated to the Middle to the Late Pleistocene. They are progressively deformed by the active fault and compose series of fault-related folds (Fo1, Fo2 and Fo3). Traces of these folds are figured out from the seismic sections obtained by this study and existing surveys. Deformation related to these folds are clearly recognized in the topography of the unit 4 base. The reliefs of strata indicate that the Fo2 fold should have uplifted seafloor at a rate of 0.09-0.20 m/ky since 300 ka. The structures, spatial distributions and growth-rates of the folds suggest that Fo1 and Fo2 should compose series of anticline developing at the front of EBFIL. Besides, Fo2 fold would compose the southern termination of the fault zone. This study has successfully demonstrated that densely operated high-resolution seismic survey can figure out distribution and activity of offshore active faults in the Late Quaternary, even at the outside of shelf.</p>

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