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| | Abstract | | Multi-channel seismic reflection method is recently found useful for physical oceanographic applications. We investigated a number of subsurface oceanic images along the same lines in Izu-Ogasawara region to compare the oceanic fine structures with different volume of source and streamer in the MCS system. The gross distribution of strong reflections agrees in all images, but we notice some sensitivity of the fine structure imaging on the different settings. |
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