沉积物结构构造随斜坡地形的类型而逐渐变化。
The sediment fabric changes gradually along this type of clinoform.
构造坡折带是指由同沉积构造长期活动引起的沉积斜坡明显突变的地带。
The structural slope_break zone, resulting in the abrupt change of the depositional slope, is initiated by the long_term activity of syndepositional structure.
精细解释表明，此类丘状体是低倾角逆断层构造、斜坡滑塌堆积及浊积扇等非礁滩沉积体的地震响应。
The accurate interpretation shows that such domal bodies are the seismic reflections of non-reef-bank deposits of low angle thrust faults, slope slump accumulative zones and turbidite fans.
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