此外，主断裂坡折带在低水位期和湖侵期，控制了沉积体系类型，而在高水位期控制了沉积体系的规模。
In addition, the main fault slop-break zone affected on the sedimentary system types during lower stand and lake transgression and on the sedimentary scale during high stand.
碳酸盐台地高水位溢流是指在海平面高水位期，台地沉积物被搬运到斜坡及较深水盆地中沉积下来所形成的沉积体。
The term "highstand shedding of carbonate platforms" means that carbonate plat forms shed most their sediments into the slopes or the formed sediments deposit into the deeper basins.
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