According to general rule, volcano eruption function from strong to weak, finally arrives the deposition, composes a volcanic eruption - depositional cycle.
根据一般规律，火山的喷发作用从强到弱，最后到沉积，组成一个火山喷发—沉积旋回。
Changes in depositional base-level cycle control the development and evolution of sequence stratigraphy.
沉积基准面旋回变化控制着陆相层序地层的形成与演化。
Moreover, the persistent depositional time and depositional rate of the high-frequency sequences are estimated based upon the information of the Milankovitch Cycle captured in the analysis.
利用捕获的米兰·科维奇周期信息，进一步计算了高频层序沉积持续的时间和沉积速率。
Depositional base-level cycle controls the development and evolution of sequence stratigraphy.
沉积基准面旋回变化控制着陆相层序地层的形成与演化。
Depositional base-level cycle controls the development and evolution of sequence stratigraphy.
沉积基准面旋回变化控制着陆相层序地层的形成与演化。
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