Therefore, the lacustrine level changes were mainly controlled by the interplay of activity rate and characteristics of the faults, transgression and the climate.

• 由于控凹断层活动的幕式性与阶段性，以及突发的海侵事件，导致湖平面升降变化轨迹为两段折线式，即快速的湖侵与缓慢的湖退。