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.
这些关系反映出构造运动的性质，是渐进的或是旋回的。
The relations reflect the nature of the tectonic movement, that is, gradual or cyclic.
重点研究和开发了利用时频分析研究沉积旋回的方法和技术。
Sedimentation cycle study method and technology using wavelet time frequency analysis theory is mostly studied and exploited.
应用推荐