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一中国位于欧亚板块的东南部,其东受太平洋板块的作用,西南受印度板块的作用,这就是施加于中国及其邻近地区的两组应力系统。因此,除了板块移动和俯冲本身是第一级的新构造运动外,中国广大地区的新构造单元布局,以及挽近构造型式的发育等等,都不能不首先归因子板块边界的活动。甚至在板块学说诞生以前,很多学者已经直觉地认识到太平洋和印度地区的活动对中国构造型式的影响和控制。例如黄汲清在一九四五年提出“古亚洲大陆”向南推进,受到太平洋的“回击力,因而形成“太平洋褶皱”;同时又受到向北挺进的冈瓦纳大陆的“抵抗”,形成了
China is located in the southeastern part of the Eurasian Plate. Its east is affected by the Pacific Plate and the Southwest by the Indian plate. This is the two sets of stress systems that are applied to China and its adjacent areas. Therefore, except the plate movement and subduction are the first-order neotectonic movements, the distribution of new tectonic units in China and the development of the Neo-Neo-Neo-Tertiary structure can not but be attributed to the activities of sub-plate boundaries in the first place. Even before the theory of plate was born, many scholars have intuitively realized the influence and control of the activities of the Pacific and India on the structure of China. For example, Huang Jiqing proposed in 1945 that “the ancient continent of Asia” advance southwards and be “hit back” by the Pacific so as to form “the Pacific Ocean fold.” At the same time, it was “resisted” by the Gondwanaland marching northward. formed