不久以前,大多数研究者认为地壳发展的主要类型只有两个——地台和地槽。地槽不同于地台和台盾,它是强烈的构造运动(包括伴有岩浆活动的运动在内)集中的地区。但在研究亚洲大陆的地质特点后,发现这里广泛发育一种特殊过程。当这种过程发生时,地台、台盾和褶皱完成区的个别部分被卷入强烈的构造运动中,并有各种各样的岩浆活动形式出现 Not long ago, most researchers thought there were only two main types of crustal development - the platform and the trough. Unlike the platform and the Taiwan shield, the trough is a region of intensive tectonic movement (including the movement associated with magmatic activity). However, after studying the geological characteristics of the Asian continent, it was found that a special process was widely developed here. As this process took place, individual parts of the platform, the Taiwan shield and the fold completion zone were involved in intense tectonic movements with various forms of magmatic activity