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多数地质学者曾经提出,亚洲大陆东缘地区中生代以后的构造运动与包括日本列岛在内的活动密切相关.最近矢野孝雄的研究又使这一观点得到了发展.他明确提出,自古生代末期峨嵋山运动直至新生代晚期岛弧运动为止的历次活动都互相关联.本文拟以上述论点为依据,对亚洲大陆东缘地区中生代后构造运动之性质与所占历史位置,从大陆地壳形成过程的阶段论来进行研究.当然,类似这样的大问题不容易解决,但是,这对于理解构造运动的某种规律性进而查明运动的机制来讲,研究这一问题是必不可少的.
Most geologists have suggested that the tectonic movement after the Mesozoic in the eastern margin of the Asian continent is closely related to the activities including the Japanese archipelago, and the recent study by Yoshihiro YOSODA has further developed this view. He made it clear that since the late Paleozoic Emei Shan All previous activities up to the Late Cenozoic island arc movement are all related to each other.On the basis of the above arguments, this paper, based on the above discussion, analyzes the nature and the historical position of the Mesozoic tectonic movement in the eastern margin of the Asian continent, Of course, a big problem like this can not easily be solved, but it is imperative to study this issue in order to understand the mechanics of constructing a regularity of motion and thus of motion.