结果表明：利用米兰柯维奇理论进行地质定年的理论依据是充分的；
The results show that the theoretical basis is practicable for geological dating using Milankovitch theory.
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。
The Milankovitch cycle, whose records in strata can be considered both as an accurate "sediment clock" and as an auxiliary dating tool, is relatively stable in the geologic history.
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