民国时期地质学研究的跨国合作——以巴尔博、李四光对中国第四纪冰川遗迹问题的争论为中心

发布时间:2019-04-13 10:08
【摘要】:中国是否存在第四纪冰川遗迹是地质学界悬而未决的重要问题,这场争论自李四光1921年宣称在华北发现相关遗迹以来,已有近百年的历史。1931年,李四光关于庐山冰川遗迹的重要发现引起了学界的广泛关注和争议,对此持怀疑态度的以苏格兰地质学家巴尔博最具代表性。作为早期中国地质事业的"客卿",巴尔博早在1920年代即来华开展了一系列的地质学研究并取得诸多成果。1934年,身在美国的巴氏再度受邀来华参加长江流域新生代地质考察,并与李四光就庐山是否存在第四纪冰川遗迹这一问题展开论辩,引起了巨大反响,这反映了地质调查所中外地质学家合作的独特模式。作为该事件的余波,1949年后李四光对此次论辩的态度出现了很大的转变,体现了政治环境的变化对地质学研究的影响。
[Abstract]:The existence of Quaternary glacier remains in China is an outstanding and important issue in the geological field. Since 1921, Li Siguang claimed to have discovered the related relics in North China, which has a history of nearly 100 years. 1931, Li Siguang's important discovery of Lushan glacier remains has aroused widespread concern and controversy in the academic community. Scottish geologist Balbo is the most representative of them. As the "guest secretary" of the early Chinese geology, Balbo came to China in the 1920s to carry out a series of geological research and made many achievements. In 1934, Pastev, who was in the United States, was again invited to China to participate in the Cenozoic geological exploration of the Yangtze River Basin. The debate with Li Siguang on the existence of Quaternary glacial relics in Lushan has caused great repercussions, which reflects the unique pattern of cooperation between Chinese and foreign geologists at the Institute of Geological Survey. As the afterwave of the event, Li Siguang's attitude to this argument changed greatly after 1949, which reflected the influence of the change of political environment on the study of geology.
【作者单位】: 中国科学院自然科学史研究所;中国科学院大学;
【基金】:中国科学院重点部署项目“地质学在中国的本土化研究”(KZZD-EW-TZ-01)的阶段性成果
【分类号】:K258

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