第四纪构造运动及现代构造形式目前可用的有关帕米尔、天山第四纪构造资料表明,现代构造形式是在较短时间内(约一百万年)形成的。当然,那时产生的强烈构造运动具有深部性,且应在莫霍面起伏上反映出来。在第四纪,这种运动的特征是方向向上和速度稳定增加。它们与新构造运动的区别为:在早第三纪末期(即约3500万年前)开始的整个新构造 Quaternary tectonic movements and modern tectonic forms Currently available on the Pamir, Tianshan Quaternary tectonic data show that the modern tectonic forms in a relatively short period of time (about one million years) formed. Of course, the strong tectonic movement that was then produced was deep and should be reflected in the Moho fluctuation. In Quaternary, this movement is characterized by a steady upward direction and upward speed. The difference between them and the neotectonic movement is that the entire new structure started at the end of the Early Tertiary (ie about 35 million years ago)