What are the four great geologists in China?
Li Siguang (1889101October 26th-1971April 29th), a Mongolian, was originally named Li Zhongmao. 1889 10 was born in a poor family in Huanggang City, Hubei Province (now Huilongshan Town, Tuanfeng County, Huanggang City, Hubei Province). Li Siguang is a world-famous scientist, geologist, educator and social activist, and one of the founders and main leaders of modern earth science and geological work in China. He studied in a private school taught by his father Li Zhuohou since childhood. 14 years old, bid farewell to his parents and came to Wuchang alone to apply for higher primary schools. When filling in the registration form, he mistook the name column for the age column, wrote down the word "fourteen", then changed the word "ten" to "Li", followed by the word "light", and from then on he got the good name of "Li Siguang". After the founding of People's Republic of China (PRC), he served as Dean of Shandong University and Head of the Department of Geology and Mineral Resources.
Liu Dongsheng
Liu Dongsheng, a famous geologist in China, is an academician of China Academy of Sciences, Third World Academy of Sciences and Eurasian Science.
Geologist Liu Dongsheng.
Academician of Chinese Academy of Sciences,1917165438+1was born in Shenyang, Liaoning Province on October 22nd. 1942 graduated from the Department of Geology, Geography and Meteorology of Southwest Associated University (Nankai University), and then took courses in the Department of Biology. From 65438 to 0944, he served as a member of the Steering Committee of China Geological Work Plan and an engineer of the Ministry of Geology, engaged in mineral exploration and engineering geology. 1949 graduated from the biology department of Nanjing University (formerly Central University). Researcher of Institute of Geology, Chinese Academy of Sciences, once served as graduate school of Peking University, Nanjing University, Sun Yat-sen University, China University of Science and Technology, and part-time professor of Jilin University. From 65438 to 0958, according to the multicycle characteristics of loess and paleosol, he found that the Quaternary climate alternated between cold and warm for far more than four times, and developed the traditional theory of four ice ages, which became a major turning point in the study of global environmental change and laid the foundation for the "multicycle theory" of environmental change.
Li Jie
(1894 ~ 1977), a geologist in China. March third. 1977 was born in cheng' an county, Hebei province on April 29th and died in Yinchuan, Ningxia on October 30th. 19 16 graduated from the College of Geology, Ministry of Agriculture and Commerce. He used to be a researcher at the Institute of Geology, Central Research Institute of Mines, Hubei Province.
Captain of production investigation team, director of Hebei Construction Department, chief engineer of Hydrogeological Engineering Geology Bureau of Ministry of Geology, chief engineer of Geology of Survey and Design Administration of Ministry of Water Resources, deputy chief engineer of General Administration of Hydropower Construction, etc. In his early years, Li Jie engaged in regional geological and mineral surveys in North China, northern Hubei, southern Henan and southern Shaanxi. He was the earliest host of Zhoukoudian Peking man excavation, and he wrote Zhoukoudian Fossil Layer in 1927. In 1930s, he made geological and mineral surveys in Hunan, Guangxi, Guizhou, Hubei, Jiangxi and other provinces. It has contributed to the development of early geological undertakings in China. In his article "Preliminary Study on Quaternary Glaciers in Western Hubei" (1940), he divided the glacial periods in the mountainous areas of western Hubei that have been used to this day. After 1949, he mainly engaged in engineering geological work in water conservancy and electric power construction, and made contributions to the construction of many reservoirs, dams and hydropower stations in China. His main works are Geology and Minerals in Zhili, Tang and Wei Counties (19 19), Geology in the Middle and South Qinling Mountains (co-authored, 1930), Geology near Jindong Temple, Luocheng, Guangxi (co-authored, 1936), etc.
Zhang hongren
Senior engineer. Zhenjiang, Jiangsu. 1952, joined the China * * * production party. 1959 graduated from the Geology Department of dnipropetrovsk Institute of Mining, USSR. He has served as the technical director of the geological team of Yunnan Provincial Geology Department, the deputy chief engineer of the Department of Geology and Mineral Resources of the Ministry of Geology, the deputy captain, deputy director and senior engineer of the Hydrogeological Engineering Geology Brigade of Beijing Geological Bureau, the director of the Hydrogeological Engineering Geology Department of the Ministry of Geology and Mineral Resources, the chief engineer of the Ministry and the deputy director of the Ministry of Geology and Mineral Resources. He has written a paper "Comparison of Numerical Methods for Solving Seepage Problems" and so on.
Professor Zhang, a geologist and representative of China, was elected as the new president of the International Union of Geosciences. This is the first time that a geologist in China has held this post.
Professor Zhang used to be the Deputy Minister of Geology and Mineral Resources of China and the Secretary-General of the Organizing Committee of the 30th International Geological Congress. He is currently a member of the Nomination Committee of the International Geological Union, a member of the Publishing Advisory Committee, and the editor-in-chief of the magazine Geological Curtain. On behalf of China, he was elected as the president of the International Geoscience Union, which fully embodies China's status as an international geological power and shows that international geosciences attach importance to the research work of geological science in China.
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Geologists and paleontologists. Hebei Quyang people. 1932 graduated from the Department of Geology of Peking University. Honorary director and researcher of Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences. In 1930s, the theory that the Sinian geosyncline distributed in a ring around and inside the polar pan-continent was put forward. At the end of 1930s, a regional geological survey was carried out in western Guangxi, which confirmed the position and characteristics of gable structure in Guangxi expounded by geomechanics theory. In the 1940s and 1950s, breakthroughs were made in the study of cephalopod fossils and Permian and Triassic strata. In his later years, he led and participated in the special research on Changxing Stratigraphy and Permian-Triassic Boundary Stratigraphy, the highest Permian in South China, and achieved fruitful results. 1980 was elected as an academician of China Academy of Sciences.