This paper puts forward a new method for the analysis of high-frequency sequences.
本文提出了进行高频层序分析的新思想和方法。
Based on the geological and geophysical data, this paper analyses characteristics and controls of high-frequency sequences of Lower Cretaceous Series in Wuerxun Depression.
利用地质、地球物理等资料对乌尔逊凹陷下白垩统高频层序特征及其控制因素进行了分析。
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。
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