沉积层序虽不同程度地受区域性构造运动和其他因素的影响，但具有明显的全球性和周期性。
We deem that the depositional sequences, though often influenced variably by local tectonics and other factors, are primarily global and periodic in nature.
某一沉积事件周期性出现的频繁程度可用时间序列中的频率来表示。
The periodic occurrence of any sedimentary event may be expressed by the frequency in the time series.
该周期控制了盆地内的沉积与剥蚀的过程及成藏旋回，并至少控制了古生代的反转构造。
All of the processes no matter what of deposition, erosion or entrapment cycles and, at least the inversion tectonics of Paleozoic, are all controlled b.
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