亚州大陆东部濒太平洋地区存在着一系列北北东向的山脉(或岛屿)和平原(或海洋),它们呈长条状的形态相互平行,间隔斜列着,构成了一个规模宏大的隆拗相间的“多”字形构造型式。李四光教授早在1929年《东亚一些典型构造型式及其对大陆运动问题的意义》一文中就已有专门研究,后来在他的许多著作中将东亚出现的这一特有的构造型式称之为“新华夏构造体系”。 There are a series of north-north-eastern mountains (or islands) and plains (or oceans) in the Pacific Ocean in the eastern part of the Asian mainland. Their elongated shapes are parallel to each other and are obliquely spaced to form a large scale Oblivious and “multi” glyph structure type. As early as 1929, Professor Li Siguang had devoted himself to the study of “Some Typical Structural Types in East Asia and Their Significance to the Problem of the Mainland Movement” in 1929, and later in many of his writings he described this peculiar structural pattern in East Asia as “ New China tectonic system. ”