摘要
概述了模拟地球内部温度结构对研究地球动力系统的重要意义，提出一个切实可行的一维热演化模型。根据该模型计算出地表幕式能量释放及其随时间的演化和地球内部温度梯度随时间的变化规律，据此探讨了地球内部能量传输机理与地质演化节律的关系，地球内部温度梯度变化和圈层分异的情况。
Firstly, this article discusses that to stimulate the Earth's temperature structure is very important for the research of the Earth's dynamic system. Secondly, an alternative one dimension model is proposed and according to this model the authors have gain the episodic energy discharge at the Earth's surface and the changeable temperature gradient within the globe. At last, the authors discuss the epoch of the Earth's evolution and the situation of substance differentiation within the Earth.
出处
《地学前缘》
EI
CAS
CSCD
1998年第A08期49-54,共6页
Earth Science Frontiers
基金
国家"九五"攀登专项
关键词
温度结构
地球动力系统
热演化模型
幕式能量释放
temperature structure, dynamic system of the Earth, thermal evolution model, episodic energy discharge
