摘要
扼要地阐述了地球发电机理论在地球深部研究中的重要地位;强调地球磁场及其时空变化是认识地球深部,尤其是核幔相互作用的主要途径;提出当前推进地球发电机理论研究的一个突破口是揭示核幔相互作用,特别是热的和化学的相互作用对地球发电机模型的影响。
Important role of the Geodynamo theory playing in the Study on the Earth' s Deep Interior in discussed briefly. The study of geomanetic field and its temporal-spatial change is one of the main tools obtaining knowlege about the Earth' s deep inferior especialy the coer-mantle interaction. It is the key to advancing the Geodynamo theory to bring to light implication of core-mantle, particularly thermal and chamical, interaction on the model of Geodynamo.
出处
《地球科学进展》
CAS
CSCD
1992年第2期31-34,共4页
Advances in Earth Science
关键词
核幔相互作用
地球发电机
地球深部
The Study on ths Earth' s Deep Interior,Core-Mantle Interaction,Geodynamo
