海底地层回波数据的成像处理是依据地层剖面仪在海面激发以及水听器接收到的海底地层声纳回波信息来研究海底地层沉积结构的一种方法。
The method of imaging the submarine sediment layers' echo data is to study the geologic structure with the information simulated by a profiler and received by hydrophone streamers at the sea surface.
变深声纳(VDS)拖航中,拖缆拖体系统偏离拖船纵中剖面的现象称为漂移。
Sometimes when a VDS is towed, the towed cable drifts off the central line of the towing ship course, this phenomenon is called towed cable kiting (or tow off).
变深声纳(VDS)拖航中,拖缆拖体系统偏离拖船纵中剖面的现象称为漂移。
Sometimes when a VDS is towed, the towed cable drifts off the central line of the towing ship course, this phenomenon is called towed cable kiting (or tow off).
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