本区深湖相沉积十分发育，并在此背景上沉积了近岸浊积扇和典型的浊积岩。
Near shore turbidite fan and typical turbidite rock are deposited on well developed deep lake facies sediments in this area.
正演模拟结果表明在时间剖面上解释的地震特征具有扇三角洲浊积岩的速度结构。
Forward modelling result indicates that seismic characteristic explained in time-section has velocity structure of fan delta-turbidite.
外扇发育远源浊积岩。
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