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| | Abstract | | Seismic reflection survey was conducted between the Ayasegawa fault and the Kazo lowland, Saitama Prefecture, central Japan to reveal the shallow subsurface structure which may control the flow of underground water. A 8.8km long CMP stacked time section is obtained after the conventional data processing. Reflectors show disturbance and gentle slope in a wider area than the flexure scarp around the Ayasegawa fault. |
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