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早在二十多年前,黄汲清教授在《中国新构造运动的几个类型》中首次将中国新构造运动划分为:1、大面积的升降运动;2、升降运动与大断裂伴生;3、翘起及断裂运动;4、拱曲运动;5、拗折、褶皱及冲断五大类型。并在论及第一类型大面积的升降运动时,明确指出,西北地区黄土高原新构造运动的特点是:“显著的幅度很大的,大面积的上升运动,自第三纪晚期以来直到现在,即在中国北方,特别在黄河流域的陕北、陇西等地区不断地进行着”。二十多年来,这些科学的论断,对中国新构造运动的研究及其类型的划分,对了解我国黄土高原地区新构造运动的特点及其表现性质等方面均起着积极的指导作
As early as more than 20 years ago, Prof. Huang Jiqing first classified the new tectonic movements in China in “Several Types of Neotectonic Movement in China” as follows: 1. Large-scale movements; 2. Up-and-down movement accompanied by large faults; 3, tilt and fracture movement; 4, bow movement; 5, bend, fold and thrust five types. And when it comes to the first type of large-scale movements, it is clearly pointed out that the new tectonic movement on the Loess Plateau in Northwest China is characterized by “significant and large-scale ascending movement, which has been occurring since the late Tertiary , That is, in northern China, especially in the Yellow River Basin in northern Shaanxi, Longxi and other areas continue to carry on. ” For more than two decades, these scientific assertions have played a positive role in guiding the study of China’s neotectonic movement and its classification, understanding the characteristics of the Neotectonic movement in the Loess Plateau, and other aspects of its performance