摘要
本文从空间——时间域模拟地壳垂直运动的观点介绍了研究地壳垂直运动的速率面拟合法。并用它研究了华北部份地区的现今地壳垂直运动。文中还将这一方法与仅从时间域来模拟地壳垂直运动的习惯做法作了简单的比较。
In this paper, A fitting method of velecity surface for vertical crustal movement research is described from the viewpoint of time-space domain modelling. And the method is used to study the present vertical crustal movements in part of North China. A brief comparision between the results obtained respectively by this method and the traditional one is also made.
出处
《地壳形变与地震》
CSCD
1989年第3期26-35,共10页
Crustal Deformation and Earthquake
基金
国家科学基金
