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  • 1
    Publication Date: 2021-05-19
    Description: The northern margin of the Philippine Sea plate is marked by the Nankai Trough. The trough is known as one of the most active seismogenic zone in the world. However, the basic observations for prediction of giagntic earthquakes such as the detailed distribution of active faults have been lacking mainly due to insufficiency of data of the detailed submarine topography. To make a more precise submarine active fault map along the trough, we have made detailed submarine topographic images based on 3 second (approximately 90 m) DEM processed from the original data obtained by Japan Coast Guard since 1984 using multi−narrow beam echo sounder. Then we have made stereo−pair copies of topographic images for interpretation of active faults, in a similar manner we use in aerial photograph stereo sets for onland active faults. We have also prepared anaglyph images from the stereo−pairs for discussion.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 83-89
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  • 2
    Publication Date: 2021-05-19
    Description: It is very regretful that we could not start our project on submarine active faults along the Japan Trench before the devastating Mw 9.0 Tohoku−Oki earthquake on March 11, 2011. Fundamental information for prediction of large earthquakessuch asthedetailed distribution of activefaultswasnotwellknown mainly due to lack of data regarding seafloor topography. To make a more precise submarine active fault map along the trench, we have made detailed seafloor topographic images based on 0.002 degree (about 150m)DEM processed from the original data obtained by Japan Coast Guard and JAMSTEC. Then we have produced anaglyph images of seafloor topography forinterpretationofactivefaults,similarinmannertohowweuseair−photostereosetsforinlandactivefaultinterpretation. Active fault distribution along and around the Japan Trench is rather simple compared with that of the Nankai Trough and/or the southwestern part of the Kuril Trench. As mapped by a previous work(Research Group for Active Faults of Japan, 2001), there are trench−parallel north−dipping thrusts. One of the extensive thrusts extends from off−Sanriku to off−Ibaraki for over 500km, and is probably related to the source fault of the 2011Tohoku− Oki earthquake. Numerous normal faults are depicted on the outer−riseslopeand they are generally short, and may cause M 7 class earthquakes.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 148-158
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  • 3
    Publication Date: 2021-05-19
    Description: We interpreted submarine landforms using anaglyph images based on 150 m DEM (Digital Elevation Model) processed from multibeam data collected by Japan Coast Guard and JAMSTEC in the area around the southwestern part of the Kuril Trench, from off Shikotan Island to Erimo Seamount, and made more precise submarine active fault maps than those produced by previous researchers. Reverse faults are mainly distributed along the northern margin of the Kuril Trench and along the foot of continental slope, while normal faults are found along the boundary of the submarine basin and the outer ridge off Kushiro. These faults are considered deeply related to large earthquakes on the plate boundary between subducting Pacific plate and Hokkaido continental mass.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.133-152 & figs
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  • 4
    Publication Date: 2021-05-19
    Description: We interpreted seafloor topography using anaglyph images based on 150 mDEM processed from multi−beam bathymetric data collected by Japan Coast Guard and JAMSTEC in the area around Nansei−Shoto Trench, and made more precise submarine active faults map than that mapped by previous workers. In the southern part of the trench, trench−parallel northwest−dipping thrusts form extensive fault scarps on the lower part of landward trench, indicating that repeated large earthquakes and tsunamis have been generated along the trench. Some of the scarps extend over several hundred km and the longest one is about 700 km. They are candidates for gigantic earthquake and tsunami generators. In the northern part, such scarps were scarcely recognized close to the trench axis due to collision of several bathymetric highs, while active reverse faults form distinctive fault scarps on the upper slope of the landward trench. They locate close to the island shelf, and are probably responsible to the uplift of islands forming Pleistocene and Holocene coastal terraces.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 133-135
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  • 5
    Publication Date: 2021-05-19
    Description: We have made detailed anaglyph images based on 150m DEM processed from the original data obtained by Japan Coast Guard and JAMSTEC, in order to analyze submarine topography for more precise interpretation of submarine active faults than that mapped by previous workers along the Sagami Trough and the Boso Triple Junction area. Younger fault escarpments on the both sides of northern part of the Sagami Trough in the Sagami Bay suggest their historical activities. In the vicinity of the Boso Triple Junction, trench−parallel west−dipping thrusts form extensive fault scarps in the aseismic gaps during historical period. One of the scarps is longer than 200km associated with evidence of repeated activity, and is probably a candidate of M 8 earthquake in not far future.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 126-129
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  • 6
    Publication Date: 2021-05-19
    Description: We have made detailed anaglyph images based on 3 second (about 90m) DEM processed from the original data obtained by Japan Coast Guard and JAMSTEC, in order to analyze submarine topography for a more precise interpretation of submarine active faults than that mapped by previous workers the eastern margin of the Sea of Japan. Most of the depicted active tectonic features are closely related to the location of symmetric anticlines formed by inversion tectonics along the former normal faults originally created during the period of formation of the Sea of Japan about 30-15 million years ago (Okamura, 2010). Interpretation of detailed anaglyph image by tectonic geomorphology method enabled us not only to depict major submarine active faults that coincide well with those revealed by the analysis of seismic reflection records, but also minor fresh tectonic landform with low−relief.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 127-144
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  • 7
    Publication Date: 2021-05-19
    Description: The distribution of subsolifluction (landslide and slope failure) along the Japan Trench, the Sagami Trough, the Suruga Trough, the Nankai Trough and the Sea of Japan is identified by 3D-image interpretation analysis using anaglyph images derived from digital bathymetry model with 90-m resolution. In order to understand the occurrence factor,( 1) the original slope of subsolifluction is restored and the distribution of slope angle is compared with surrounding slopes, (2) the relation between area of subsolifluction versus frequency is discussed from a viewpoint of power-law model and (3) the location of subsolifluction is investigated with distribution of active faults. The result shows that the incentive factor of strong ground motion by earthquakes contributes more to large subsolifluction than the basic factor of slope angle.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.1-16
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  • 8
    Publication Date: 2021-05-19
    Description: We have made detailed anaglyph images of the Izu‒Ogasawara Trench and its vicinity based on 150 m DEM(Digital Elevation Model) processed from the original data obtained by Japan Coast Guard and JAMSTEC, in order to provide more detailed 3D submarine images for a more precise interpretation of tectonic landforms than previous studies. We give examples of images of the plate boundary around Mogi Seamount, extensive submarine eruption around Sumisu Caldera, normal faulting around Shichiyo Volcano Chain, volcanic domes between Sofugan Tectonic Line and Sofu Trough, central part of the Ogasawara Ridge and normal faulting around the Ogasawara Plateau.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 140-157
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