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Li Siguang, formerly known as Li Zhonghua, is a world-renowned scientist, geologist, educator and social activist, and the founder of modern earth science and geological work in China. He was born on October 26, 1889 in Huanggang County, Hubei Province, and died in Beijing on April 29, 1971.
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Li Siguang, formerly known as Zhong Kui, born on October 26, 1889, is a paleontologist, stratigrapher, geotectonist, Quaternary glaciologist and geologist. Mongolian. A native of Huanggang, Hubei.
He received his master's degree and doctorate degree from the University of Birmingham in 1919 and 1927, respectively. He has studied in Japan and the United Kingdom. In his early years, he joined the League and participated in the Xinhai Revolution.
He used to be a professor of the Department of Geology of Peking University and the director of the Institute of Geology of the ** Research Institute. On October 19, 1949, while still adrift, he was appointed vice president of the Chinese Academy of Sciences. After returning to China, he served as the Minister of Geology and the Chairman of the China Association for Science and Technology for a long time.
Li Siguang has served as the first.
Vice Chairman of the 2nd, 3rd and 4th National Committee of the Chinese People's Political Consultative Conference, Minister of Geology, Vice President of the Chinese Academy of Sciences, Chairman of the China Association for Science and Technology, Vice Chairman of the World Association of Scientists. On April 29, 1971, Li Siguang died of illness at the age of 82.
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Li Siguang (1889-1971), Mongolian, whose name was Zhonggong, was born on October 26, 1889 in a poor family in Huanggang County, Hubei Province. He is a world-renowned scientist, geologist, educator and social activist, and the founder of modern earth science and geological work in China. He studied in the private school taught by his father Li Zhuohou since he was a child, and when he was 14 years old, he said goodbye to his parents and came to Wuchang alone to apply for the higher primary school.
When filling out the registration form, he mistakenly took the name column as the age column, wrote down the words "fourteen", and then changed the "ten" to "Li", and added the word "light" after it, and since then he has been famous as "Li Siguang" in the world.
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Li Siguang is the father of Chinese geology.
Li Siguang is one of the important pioneers of China's geological work, he is the founder of China's geomechanics, he is known as the "father of Chinese geology" Li Siguang, the father of China's geology Li Siguang has made great contributions to China's geological exploration for many times.
Li Siguang's achievements
In August 1951, Li Siguang was appointed as the newly established dean of the Northeast Institute of Geology. Under the leadership of Li Siguang, the Northeast Institute of Geology has cultivated a large number of technical personnel for geological exploration and scientific research in the future, and met the needs of the country's geological development.
In 1952, Li Siguang was transferred back to the Institute of Geology of the Chinese Academy of Sciences. In September of the same year, Li Siguang was appointed Minister of Geology of the People's Republic of China.
In August 1958, Li Siguang was appointed chairman of the Atomic Energy Commission. During his tenure, Li Siguang used his knowledge of geomechanics theory to guide technicians to discover a series of uranium deposits, which ensured the development needs of China's nuclear industry and made great contributions to the development of China's nuclear industry.
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Discovery of Quaternary glaciers.
During his research on fossils in the family Cypteridae, Li Siguang discovered some stones that resembled glacial stripes at the eastern foot of Taihang Mountain. He continued to investigate the Datong Basin, and became more and more convinced of his own judgment, so he boldly put forward the view of the existence of Quaternary glaciers in China at the third general meeting of the Geological Society of China. Andersen, a Swedish geologist and adviser to the Ministry of Agriculture and Commerce, smiled contemptuously and denied it.
In order to make people acceptable to this fact, he continued to search for more glacial remains. Ten years later, he not only concluded that there were a large number of glacial relics in Lushan, but also believed that China's Quaternary glaciers were mainly valley glaciers and could be classified as three glacial periods. When Li Siguang's academic views were published again at the National Geological Society, it caused the famous Lushan debate in 1934.
In the old semi-feudal and semi-colonial China, Chinese scientists were inferior, and a considerable number of foreign scholars came to China with nationalist and racist sentiments. Thus, despite the abundance of facts in front of them, several foreign scholars have not changed their views. In 1936, Li Siguang went to Huangshan again to investigate, and wrote "The Quaternary Glacial Phenomenon of Huangshan in Anhui Province", this article and several glacial phenomena attracted the attention of some Chinese and foreign scholars
It was a seismic discovery. "Li Siguang's hard work for more than 10 years has been publicly recognized by foreign scientists for the first time. However, he knew that this was not enough, so he simply moved his family to Lushan Mountain, and established a glacier exhibition hall at the foot of Lushan Mountain, named "Baishi Exhibition Hall" (later blown up by the Kuomintang Navy) to conduct more in-depth and detailed glacier research.
Li Siguang's many years of research on glaciers were comprehensively expounded in Lushan in the Ice Age, which was completed in 1937. Unfortunately, due to the outbreak of the Anti-Japanese War, this book was not published until 10 years later.
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On April 29, 1971, Li Siguang died of illness at the age of 82.
Li Siguang (, character Zhonggong, formerly known as Li Zhongjiao, a native of Huanggang, Hubei, Mongolian, geologist, educator, ** family and social activist, is the founder of Chinese geomechanics, one of the main leaders and founders of China's modern earth science and geological work, the first batch of outstanding scientists after the founding of New China and the father of the founding of New China who made outstanding contributions, and was elected as one of the 100 moving Chinese people since the founding of New China in 2009.
Li Siguang graduated from Osaka Higher Technical School in Japan in July 1910; In 1911, he served as the Minister of Industry of the Hubei Army; In January 1928, he was appointed as the director of the Institute of Geology of the ** Research Institute; In 1948, he was elected as an academician of the ** Research Institute; In May 1950, he was appointed Vice President of the Chinese Academy of Sciences. In April 1951, he was elected Vice Chairman of the Executive Committee of the World Association of Scientists. In September 1952, he was appointed Minister of Geology of the People's Republic of China; In 1955, he was elected as a member (academician) of the Chinese Academy of Sciences; In September 1958, he was appointed as the chairman of the China Association for Science and Technology; In April 1969, he was elected as a member of the 9th ** Committee of the Communist Party of China; In August 1970, he served as the head of the science and education group.
Li Siguang founded geomechanics and made important contributions to the development of China's petroleum industry. In the early years, he had superb research on the fossils of the Flyflies and their stratigraphic significance, put forward the existence of Quaternary glaciers in eastern China, established the concepts of "geomechanics" and "tectonic system" in the new marginal disciplines, established the concept of "tectonic system", and founded the school of geomechanics. This paper proposes the understanding of the broad prospect of oil prospecting in the three subsidence zones of the New China tectonic system, and creates a forecasting method that combines active tectonic research and in-situ stress observation.
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October 26th.
Li Siguang's birthday (accurate).
Recommended Answer: Li Siguang (1889, 1971) was born on October 26, 1889.
Chinese geologist, paleontologist, glaciologist, political activist. Academician of the Chinese Academy of Sciences. Mongolian.
Born in 1889 in Huanggang, Hubei. He died in Beijing on April 29, 1971. In 1905, he studied shipbuilding at the Osaka Institute of Technology in Japan, and in 1912 he went to the University of Birmingham in the United States to study geology, and received a master's degree in geology in 1919 and a doctorate in science in 1927.
He returned to China in 1949. He has successively served as Minister of Geology of the People's Republic of China, Vice President of the Chinese Academy of Sciences, Director of the Institute of Paleontology of the Chinese Academy of Sciences, Chairman of the China Association for Science and Technology, Head of the Science and Education Group, and Vice Chairman of the World Association of Scientists. Member of the Standing Committee of the First National Committee of the Chinese National Committee of the Chinese People's Political Consultative Conference.
Vice-Chairman of the 2nd, 3rd and 4th National Committee. He has been engaged in the research and teaching of geology for a long time and has made great contributions. His masterful study of fossils laid the foundation for the demarcation, stratification and contrast of the marine Carboniferous Permian strata.
The existence of Quaternary glaciers in China was proposed. He used the perspective of mechanics to study the phenomenon of crustal movement, explored the law of crustal movement and mineral distribution, regarded various tectonic traces as the result of in-situ stress activities, and established the concept of tectonic system, thus creating a new marginal discipline of geomechanics. In practice, he analyzed the characteristics of geological structures in eastern China, and believed that the three subsidence zones of the New China tectonic system have broad prospects for oil searching.
The successive discoveries of oil fields such as Daqing, Shengli, and Dagang confirmed his scientific conclusion. In terms of forecasting, it is emphasized that on the basis of studying the activity of geological structure, the method of observing in-situ stress should be used to explore the way of forecasting. He has superb research and deep attainments in the basic disciplines of geology, such as stratigraphy, structural geology, paleontology, quaternary glaciology, petrology, mineralogy, etc.
He is the author of "The Main Causes of the Change of the Earth's Surface Image", "Introduction to Geomechanics", "**Geology" and the anthology "Astronomy, Geology, Paleontology".
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Li Siguang is a famous Chinese geologist, the first batch of outstanding scientists after the founding of the People's Republic of China and the father who made outstanding contributions to the development of New China, the first president of China University of Geosciences, and a native of Huanggang, Hubei.
Li Siguang graduated from the University of Birmingham with a Ph.D. degree. Pioneered geomechanics. **Academician of the Research Institute, academician of the Chinese Academy of Sciences, and later Li Siguang's famous deeds were also remade into movies.
In 1932, he was appointed president of **university**, and later served as a professor at Chongqing Liquid Disturbance University. It has made significant contributions to China's shaking off the "oil-poor" hat, establishing the theory of geomechanics and the research and development of China's "two bombs".
Li Siguang (1889-1971) was a Chinese geologist and the founder of geomechanics. The word Zhonghua is a native of Huanggang, Hubei. In his early years, he joined the League and participated in the Xinhai Revolution. >>>More
Li Siguang (1889-1971) was a Chinese geologist and the founder of geomechanics. The word Zhonghua is a native of Huanggang, Hubei. In his early years, he joined the League and participated in the Xinhai Revolution. >>>More
Geologist. Scientist.
Elderly. >>>More
There are a large number of remnants of Quaternary glacial activity in the Yangtze River basin. >>>More