关于地球圈层差异旋转理论研究的综述  

A Survey: the Theoretical Study of Differential Rotation Between Layers Inside the Earth

作　　者：张中信[1] 陈殿有 周菊仙 

机构地区：[1]长春科技大学应用理学院,长春130026 [2]山西省地矿局区调队实验室,榆次030600

出　　处：《世界地质》1997年第4期59-62,共4页World Geology

摘　　要：地球内部各圈层差异旋转的各种假说中，“内快外慢”说已形成较完整的理论，并被科学测试所验证。在这一理论形成过程中，数学工作者也做出了有益的贡献。研究表明，“内快外慢”差异旋转是地球内部各种运动的源动力。这一理论的价值还在于，它不仅可以解释各种地质现象，而且促进了地球内部能量的积累和释放的研究、地质旋回与天文周期相关关系的研究、全球气候变化的研究等。On the study of differential rotation between layers inside the earth therepresented various hypotheses and among these the hypothesis, it is 'Inner Fast and OuterSlow' that has recently evolved into an increasingly accepted theory, and moreover, it isverified by data obtained from sicentific obervation. In the process of the formation of 'Inner Fast and Outer Slow' theory, mathematicians concerned have also made their indispensable contribution. Their contribution lies in the discovery that differential rotationinner fast and outer slow consitututes the initial power for the various motions inside theearth. The mathematicians' work also helps us to interpret various geologic phenomenaand to advance researches in energy accumulation and release inside the earth, in understanding the relationship between geologic cycle and astronomical period, and in global climate change.

关 键 词：圈层差异旋转 天文周期 地质旋回 地球圈层 

分 类 号：P183.2[天文地球—天文学]