论文部分内容阅读
陈国达院士 陈国达,男,汉族,1912年出生,广东省新会县人,1934年毕业于中山大学地质系。 陈国达教授是世界著名的地质学家,现任中南工业大学学术顾问、一级教授、博士生导师,中国科学院长沙大地构造研究所名誉所长,1980年当选为中国科学院学部委员(现称院士)。 陈国达教授最突出的贡献是于1956年发现大陆地壳的新构造单元——地洼区,并在此基础上创建了壳体大地构造学,发展成为地洼(活化)构造理论体系,在国内外广泛运用于找矿取得显著成效。地洼学说
Chen Guoda Academician Chen Guoda, male, Han nationality, born in 1912 in Xinhui County, Guangdong Province, graduated from Zhongshan University Department of Geology in 1934. Professor Chen Guoda is a world famous geologist. He is currently an academic advisor, a professor and a doctoral tutor at South Central University of Technology. He was honorary director of the Changsha Institute of Tectonics and Geophysics, Chinese Academy of Sciences. In 1980, he was elected academician (now academician) of the Chinese Academy of Science. Professor Chen Guoda’s most prominent contribution was discovered in 1956, the new tectonic unit of the continental crust - Diwa, and on this basis to create a shell tectonics, developed into the depression (activation) tectonic theory system at home and abroad Widely used in prospecting to achieve remarkable results. Diwa theory