并且隔层和沉积相的分布规律受沉积旋回的控制。
And the distribution of barriers and facies were controlled by the deposit cycles.
沉积基准面旋回变化控制着陆相层序地层的形成与演化。
Changes in depositional base-level cycle control the development and evolution of sequence stratigraphy.
这些泥岩和页岩在湖相高频旋回中的变化相当复杂。
The variety of these mudstone and shales is very complex in lacustrinehigh-frequency cycle.
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