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1998-2000 Hokkaido Transect Seismic Refraction/
Wide-angle Reflection Line Seismic Reflection Line Multi-disciplinary Project Large scale structural variation from NJA to KA Deeper structure of Hidaka Collision Zone 3D crustal inhomogeneity Features of crustal activity
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1. Reflection Analysis CRS (Common Reflection Surface Method) and
MDRS (Multi-dip Reflection Surfaces Method)
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H HMT W E Conventional (CMP stacking) CRS/MDRS stacking
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Hidaka 99 Iwasaki et al. (2004)
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S3002 (1999 Seismic Line) Fault zone
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