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米兰柯维奇旋回在地质历史时期具有相对的稳定性，其在地层中的记录可以作为一座精确的“沉积物钟”和辅助的测龄工具．利用小波分析从测井曲线中识别米氏旋回，可以确定地层沉积的持续时间．通过与其他方法定年结果比较，表明该方法具有一定的准确性和可靠性，并且它还可应用于其他碎屑岩地区
The Milankovitch cycle is relatively stable during geological history and its record in the formation can be used as an accurate “sediment clock” and as a secondary measuring tool. Using wavelet analysis to identify Mie cycles from well logs, the duration of formation deposition can be determined. Compared with the results of other methods, the results show that the method has certain accuracy and reliability, and it can also be applied to other clastic areas