中国地壳构造的发生、发展及演化进程,是受它所处的世界大地构造的特殊位置所决定的。由于中国陆壳位于黄汲清教授划分的古亚洲构造域、特提斯-喜马拉雅构造域及滨太平洋构造域的交织迭置区域中,因此各构造域的构造活动,均将影响波及到中国幅员范围的地壳。甚至彼此互相交织、迭置和改造,而酿成中国地质构造的复杂多样 The occurrence, development and evolution of crustal structure in China are determined by the special position of the world earth in which it is located. Since the continental crust in China is located in the inter-overlapping area of ​​the ancient Asian tectonics, the Tethys-Himalayas tectonics and the Pacific Rim tectonic domain divided by Professor Huang Jiqing, the tectonic activity of each tectonic domain will affect the amplitude Range of the crust. Even intertwined with each other, overlapping and transformation, and lead to China’s geological structure of the complex and diverse