地壳板块构造运动学说最近又获得新的证实。这个由德国地球物理学家A·魏格纳1912年提出并经各国科学家充实完善的大陆漂移理论认为,组成地壳的各个部分处于明显而不断的运动之中。对地壳板块相互位置及其运动进程的实验性观察大约开始于15年前,观察的基本方法是对来自遥远宇宙天体(类星体)的无线电讯号进行同步接收。此项研 Crustal plate tectonics kinematics recently gained new confirmation. This theory of continental drift, proposed by German geophysicist A. Weggner in 1912 and enriched by scientists from all over the world, holds that the various parts of the crust are in a clear and constant movement. The experimental observation of the mutual position of the crustal plates and their movement began approximately 15 years ago and the basic method of observation was the simultaneous reception of radio signals from distant cosmic bodies (quasars). This research