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地球科学进展  1992, Vol. 7 Issue (2): 31-    DOI: 10.11867/j.issn.1001-8166.1992.02.0031
学科发展与研究     
核慢相互作用与地球发电机理论
马石庄 魏青云 徐文耀
中国科学院地球物理研究所 100101
ON THE CORE-MANTLE INTERACTION AND GEODYNAMO THEORY
Ma Shizhuang,Wei Qingyun,Xu Wenyao
Institute of Geoyhysics,  Chinese Academy of Sciences,Beijing  100101
 全文: PDF(1041 KB)  
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,尤其是核慢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慢相互作用,特别是热的和化学的相互作用对地球发电机模型的影响。   

关键词: 地球深部研究核慢相互作用地球发电机    
Abstract:

   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 interior especialy the coer一mantle interabtion. 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.

Key words: The Study on the Earth' s Deep Interior    Core-Mantle Interaction    Geodynamo
收稿日期: 1991-04-20 出版日期: 1992-03-01
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引用本文:

马石庄 魏青云 徐文耀. 核慢相互作用与地球发电机理论[J]. 地球科学进展, 1992, 7(2): 31-.

Ma Shizhuang,Wei Qingyun,Xu Wenyao. ON THE CORE-MANTLE INTERACTION AND GEODYNAMO THEORY. Advances in Earth Science, 1992, 7(2): 31-.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.1992.02.0031        http://www.adearth.ac.cn/CN/Y1992/V7/I2/31


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