中国是以大陆为主的国家,广泛存在不同时代、不同方向、不同结构、不同性质的造山带,也有中新生代在陆壳基底上因裂解扩张形成的南海盆地。对这些地区进行深入研究,将为建立中国大陆构造理论提供地质基础和重要条件。20世纪30年代始,中国老一辈构造地质学家通过对中国大陆构造研究,陆续创立了不同构造学派,促进了对中国大陆构造研究的深入和发展。自20世纪70年代初, As a continent-dominated country, China has widespread orogenic belts of different ages, directions, structures and properties, and also formed the Meso-Cenozoic South China Sea basin formed by pyrolysis and expansion on the continental crust. An in-depth study of these areas will provide the geological basis and important conditions for the establishment of the tectonic theory in mainland China. Since the 1930s, China’s older tectonic geologists have successively established different schools of tectonics through the study of the tectonics in mainland China, which has promoted the further development of tectonic researches in mainland China. Since the early 1970s,